Sample ID|Original Sample ID|Primary Reference|Secondary Reference|Sample date (day.month.year)|Type of Sample|Location description|ISNET X (m)|ISNET Y (m)|Longitude (decimal degrees)|Latitude (decimal degrees)|Elevation (m.a.s.l.)|Depth (m)|Sample description (Icelandic) |Sample description (English)|Broad lithological category|Lithological identifier|Alteration zone|Grain density (g cm-3)|Remarks - grain density|Total porosity (-)|Remarks - total porosity|Connected porosity (-)|Remarks - effective porosity|Intrinsic permeability (m2)|Remarks - intrinsic permeability|Liquid apparent permeability (m2)|Remarks - liquid apparent permeability|Gas apparent permeability (m2)|Remarks - Gas apparent permeability|Bulk resistivity (?m)|Bulk conductivity (S m-1)|Surface Conductivity (S m-1)|Fluid Conductivity (S m-1)|Formation Resistivity Factor (-)|Cation Exchange Capacity (C g-1)|Electrical resistivity measurement type and remarks|P-wave velocity, dry (km s-1)|P-wave velocity, saturated (km s-1)|S-wave velocity, dry (km s-1)|S-wave velocity, saturated (km s-1)|Poisson's ratio (-)|Uniaxial compressive strength (MPa)|Young modulus coef. (GPa)|Shear modulus coef. (GPa)|Tensile strength (Mpa)|Thermal conductivity (W m-1 K-1)|
Palsson1984_1|P-1|Pálsson et al., 1984|Pálsson et al., 1972|4.10.1969|Borehole|Reykjanes H-8 (RN-08)|319054|374424|-22.67677|63.82637|29|1373|Ummyndađ set|Altered sediment|Sediment|Sediment|Altered|2.82|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_2|P-2|Pálsson et al., 1984|Pálsson et al., 1972|18.6.1969|Borehole|Reykjanes H-6 (RN-06)|317568|373067|-22.70527|63.81343|27|571|Ummyndađ ţursaberg|Altered agglomerate|Hyaloclastite|Hyaloclastite breccia|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.220|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_3|P-3|Pálsson et al., 1984|Pálsson et al., 1972|18.6.1969|Borehole|Reykjanes H-6 (RN-06)|317568|373067|-22.70527|63.81343|27|302|Ummyndađ ţursaberg|Altered agglomerate|Hyaloclastite|Hyaloclastite breccia|Altered|2.81|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_4|P-4|Pálsson et al., 1984|Pálsson et al., 1972|17.5.1969|Borehole|Ártúnshöfđi G-32 (R-32)|366771|400934|-21.81140|64.12735|40|850|Dólerít|Dolerite|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Unaltered|3.19|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_5|P-5|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1963|Borehole|Skyggnir viđ Elliđavatn H-38|361791|405232|-21.79133|64.09547|75|29|Grágrýti|Olivine tholeiite lava  |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_6|P-6|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1963|Borehole|Skyggnir viđ Elliđavatn H-38|361791|405232|-21.79133|64.09547|75|209|Grágrýti|Olivine tholeiite lava   |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_7|P-7|Pálsson et al., 1984|Pálsson et al., 1972|3.10.1961|Borehole|Húsavík H-1 (HU-1)|574690|618652|-17.35140|66.05543|57|954|Leirsteinn|Mudstone, siltstone|Sediment|Sediment|Unaltered|2.91|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.157|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_8|P-8|Pálsson et al., 1984|Pálsson et al., 1972|3.10.1961|Borehole|Húsavík H-1 (HU-1)|574690|618652|-17.35140|66.05543|57|1052|Leirsteinn|Mudstone, siltstone|Sediment|Sediment|Unaltered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.163|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_9|P-9|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíđarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|240|Fínkornótt sjávarset|Fine-grained sea sediment|Sediment|Sediment|Unaltered|2.77|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.433|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.397|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_10|P-10|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíđarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|640|Fremur grófkristallađ storkuberg međ fylltum sprungum|Rather coarsely crystalline igneous rock with filled vesicles|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.143|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_11|P-11|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíđarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|1010|Títanágítbasalt og molaberg|"Titanite-augite-rich basalt and ""conglomerate"""|Sediment|Sediment|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.767|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.023|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_12|P-12|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíđarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|1517|Basalt međ fylltum sprungum|Basalt with filled veins|Basaltic intrusion|Fine-medium grained basaltic intrusion|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.533|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.043|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_13|P-13|Pálsson et al., 1984|Pálsson et al., 1972|4.10.1969|Borehole|Reykjanes H-8 (RN-08)|319054|374424|-22.67677|63.82637|29|1369|Ummyndađ set|Altered sediment|Sediment|Sediment|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_14|P-14|Pálsson et al., 1984|Pálsson et al., 1972|27.5.1964|Borehole|Gufunes (H-40)|372791|408363|-21.82013|64.15055|4|173|Međalblöđrótt basalt|Medium-vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_15|P-15|Pálsson et al., 1984|Pálsson et al., 1972|11.2.1965|Borehole|Seltjarnarnes H-2 (SN-02, HS-02)|356605|407165|-22.00570|64.16130|2|80|Stórblöđrótt basalt|Basalt with large vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_16|P-16|Pálsson et al., 1984|Pálsson et al., 1972|4.1.1965|Borehole|Seltjarnarnes H-1 (SN-01, HS-01)|356600|407160|-22.00335|64.15105|4|52|Ţursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.360|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_17|P-17|Pálsson et al., 1984|Pálsson et al., 1972|4.1.1965|Borehole|Seltjarnarnes H-1 (SN-01, HS-01)|356600|407160|-22.00335|64.15105|4|77|Blöđrulítiđ basalt|Basalt with minor vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_18|P-18|Pálsson et al., 1984|Pálsson et al., 1972|4.1.1965|Borehole|Seltjarnarnes H-1 (SN-01, HS-01)|356600|407160|-22.00335|64.15105|4|93|Ţursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_19|P-19|Pálsson et al., 1984|Pálsson et al., 1972|26.2.1967|Borehole|Akranes ST-2|351375|428082|-22.07411|64.32246|1|83|Blöđrótt basalt|Vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_20|P-20|Pálsson et al., 1984|Pálsson et al., 1972|26.2.1967|Borehole|Akranes ST-2|351375|428082|-22.07411|64.32246|1|98|Stórblöđrótt basalt međ holufyllingum|Basalt with large vesicles. Some infillings|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.290|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_21|P-21|Pálsson et al., 1984|Pálsson et al., 1972|26.2.1967|Borehole|Akranes ST-2|351375|428082|-22.07411|64.32246|1|30|Rauđleitt völuberg|Oxidized conglomerate|Sediment|Sediment|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.237|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.233|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_22|P-22|Pálsson et al., 1984|Pálsson et al., 1972|26.2.1967|Borehole|Akranes ST-2|351375|428082|-22.07411|64.32246|1|49|Basalt|Basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.147|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_23|P-23|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerđishreppi H-1 (SH-1)|404420|382050|-20.94852|63.92876|20|35|Blöđrótt basalt, nokkuđ holufyllt|Vesicular basalt, partly vesicle-filled|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_24|P-24|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerđishreppi H-1  (SH-1)|404420|382050|-20.94852|63.92876|20|58|Rauđleitt, blöđrulaust basalt|Oxidized, compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_25|P-25|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerđishreppi H-1  (SH-1)|404420|382050|-20.94852|63.92876|20|68|Blöđrulaust basalt|Compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.550|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_26|P-26|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerđishreppi H-1  (SH-1)|404420|382050|-20.94852|63.92876|20|73|Völuberg|Conglomerate|Sediment|Sediment|Unaltered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.310|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_27|P-27|Pálsson et al., 1984|Pálsson et al., 1972|8.4.1967|Borehole|Kaldárholt í Holtum H-1 (KH-01)|429114|388170|-20.44816|63.98958|57|46|Basalt međ strjálum dálítiđ holufylltum blöđrum|Basalt with minor vesiculation and slightly filled vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_28|P-28|Pálsson et al., 1984|Pálsson et al., 1972|8.4.1967|Borehole|Kaldárholt í Holtum H-1 (KH-01)|429114|388170|-20.44816|63.98958|57|58|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_29|P-29|Pálsson et al., 1984|Pálsson et al., 1972|24.11.1969|Borehole|Stardalur H-1 (SD-01)|379501|414357|-21.48190|64.21055|187|42|Grćnleitt, fínkornótt set|Green-colored fine-grained sediment|Sediment|Sediment|Unaltered|2.88|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_30|P-30|Pálsson et al., 1984|Pálsson et al., 1972|24.11.1969|Borehole|Stardalur H-1 (SD-01)|379501|414357|-21.48190|64.21055|187|61|Blörulaust basalt|Compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_31|P-31|Pálsson et al., 1984|Pálsson et al., 1972|27.8.1969|Borehole|Námafjall H-8 (B-8)|599073|573121|-16.84775|65.64073|333|540|Ummyndađ bólstraberg|Altered pillow lava|Hyaloclastite|Pillow basalt|Altered|2.93|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.155|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.125|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_32|P-32|Pálsson et al., 1984|Pálsson et al., 1972|27.8.1969|Borehole|Námafjall H-8 (B-8)|599073|573121|-16.84775|65.64073|333|540|Líparít|Rhyolite|Silicic volcanic|Rhyolite lava|Unaltered|2.69|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.123|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.107|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_33|P-33|Pálsson et al., 1984|Pálsson et al., 1972|27.8.1969|Borehole|Námafjall H-8 (B-8)|599073|573121|-16.84775|65.64073|333|540|Bólstraberg|Pillow lava|Pillow basalt|Pillow basalt|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.195|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_34|P-34|Pálsson et al., 1984|Pálsson et al., 1972|6.7.1970|Borehole|Nesjavellir H-4 (NV-04)|499510|324275|-21.26780|64.10295|232|250|Blöđrótt, mjög fínkornótt basalt|Vesicular, very fine-grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_35|P-35|Pálsson et al., 1984|Pálsson et al., 1972|6.7.1970|Borehole|Nesjavellir H-4 (NV-04)|499510|324275|-21.26780|64.10295|232|250|Mjög fínkornótt basalt|Very fine-grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.220|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_36|P-36|Pálsson et al., 1984|Pálsson et al., 1972|6.7.1970|Borehole|Nesjavellir H-4 (NV-04)|499510|324275|-21.26780|64.10295|232|250|Fínkornótt basalt|Fine-grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_37|P-37|Pálsson et al., 1984|Pálsson et al., 1972|6.7.1970|Borehole|Nesjavellir H-4 (NV-04)|499510|324275|-21.26780|64.10295|232|250|Blöđrótt, mjög fínkornótt basalt|Vesicular, very fine-grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.360|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.350|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_38|P-38|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 1|392508|393330|-21.19915|64.02639|102||Dökkgrćnleitt túff međ kalsíteitlum|Dark green tuff with calcite|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.83|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.260|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.260|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_39|P-39|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 2|392508|393330|-21.19915|64.02639|102||Grćnt túff|Green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.355|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.350|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_40|P-40|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 3|392508|393330|-21.19915|64.02639|102||Fínkornótt basalt úr gangi|Fine-grained basalt from dyke|Basaltic intrusion|Fine-medium grained basaltic intrusion|Unaltered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_41|P-41|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 4|392508|393330|-21.19915|64.02639|102||Grćnleitt túff međ brúnum og gráum eitlum|Green-colored tuff with brown and gray precipitates|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.82|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_42|P-42|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 5|392508|393330|-21.19915|64.02639|102||Súrt, straumlögótt gangberg međ miklu af pýríti|Acidic, flow-banded dyke with abundant pyrite|Intermediate intrusion|Diorite|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_43|P-43|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 6|392508|393330|-21.19915|64.02639|102||Grćnleitt, ummyndađ berg|Green-colored, altered rock|Hyaloclastite|Hyaloclastite tuff|Altered|2.76|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_44|P-44|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 7|392508|393330|-21.19915|64.02639|102||Ljósgrćnt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.300|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_45|P-45|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 8|392508|393330|-21.19915|64.02639|102||Grćnrauđleitt basalt međ miklu af pýríti|Green-red basalt with abundant pyrite|Lava flow|Fine-medium grained basaltic lava|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_46|P-46|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 9|392508|393330|-21.19915|64.02639|102||Fínkornótt basalt|Fine-grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.015|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_47|P-47|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Grćndalsá ofan Reykjakots í Ölfusi nr. 10|392508|393330|-21.19915|64.02639|102||Ljósgrćntleitt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.210|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.190|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_48|P-48|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur A|393140|392391|-21.18559|64.01816|84||Grćnleitt túff međ hvítum dílum|Green-colored tuff with white precipitates (or phenocrysts)|Hyaloclastite|Hyaloclastite tuff|Altered|2.80|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_49|P-49|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur B|393140|392391|-21.18559|64.01816|84||Ljósgrćnt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.310|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.300|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_50|P-50|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur C|393140|392391|-21.18559|64.01816|84||Brúnt túff|Brown tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.80|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.270|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_51|P-51|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur D í sömu opnu og C, en 2 m neđar|393140|392391|-21.18559|64.01816|84||Grćnleitt ţursaberg|Green-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.75|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.115|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_52|P-52|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur E í 10 m lárétti fjarlćgd frá D|393140|392391|-21.18559|64.01816|84||Grćnbrúnt molaberg|Green-brown sedimentary rock|Sediment|Sediment|Unaltered|2.86|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.240|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_53|P-53|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Sauđá ofan Reykjakots í Ölfusi stađur F|393140|392391|-21.18559|64.01816|84||Ljósgrćnt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.77|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_54|P-54|Pálsson et al., 1984|Pálsson et al., 1972|16.4.1970|Borehole|Hrauneyjar HP-3|488338|409818|-19.23996|64.19087|475|13|Smáblöđrótt basalt, kubbaberg|Cube-jointed basalt, small vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.230|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_55|P-55|Pálsson et al., 1984|Pálsson et al., 1972|16.4.1970|Borehole|Hrauneyjar HP-3|488338|409818|-19.23996|64.19087|475|30|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Pillow basalt|Pillow basalt|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_56|P-56|Pálsson et al., 1984|Pálsson et al., 1972|16.4.1970|Borehole|Hrauneyjar HP-3|488338|409818|-19.23996|64.19087|475|31|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Pillow basalt|Pillow basalt|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.220|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_57|P-57|Pálsson et al., 1984|Pálsson et al., 1972|16.4.1970|Borehole|Hrauneyjar HP-3|488338|409818|-19.23996|64.19087|475|32|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Pillow basalt|Pillow basalt|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_58|P-58|Pálsson et al., 1984|Pálsson et al., 1972|16.4.1970|Borehole|Hrauneyjar HP-3|488338|409818|-19.23996|64.19087|475|44|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Pillow basalt|Pillow basalt|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.340|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.260|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_59|P-59|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|4|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_60|P-60|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|8|Ţétt, stórdílótt basalt|Dense porphyritic basalt|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_61|P-61|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|12|Blöđrulítiđ, stórdílótt basalt|Porphyritic basalt with small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_62|P-62|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|18|Međalblöđrótt, stórdílótt basalt|Porphyritic basalt with medium-vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_63|P-63|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|20|Fremur blöđrulítiđ, stórdílótt basalt|Porphyritic basalt with minor vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_64|P-64|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|21|Fremur blöđrulítiđ, stórdílótt basalt|Porphyritic basalt with minor vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_65|P-65|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-4|488480|409135|-19.23698|64.18473|420|23|Međalblöđrótt, stórdílótt basalt|Porphyritic basalt with medium vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_66|P-66|Pálsson et al., 1984|Pálsson et al., 1972|25.7.1970|Borehole|Hrauneyjar HP-10|487896|409499|-19.24903|64.18798|446|6|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.310|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_67|P-67|Pálsson et al., 1984|Pálsson et al., 1972|25.7.1970|Borehole|Hrauneyjar HP-10|487896|409499|-19.24903|64.18798|446|10|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_68|P-68|Pálsson et al., 1984|Pálsson et al., 1972|25.7.1970|Borehole|Hrauneyjar HP-10|487896|409499|-19.24903|64.18798|446|11|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.230|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_69|P-69|Pálsson et al., 1984|Pálsson et al., 1972|25.7.1970|Borehole|Hrauneyjar HP-10|487896|409499|-19.24903|64.18798|446|19|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_70|P-70|Pálsson et al., 1984|Pálsson et al., 1972|25.7.1970|Borehole|Hrauneyjar HP-10|487896|409499|-19.24903|64.18798|446|23|Smáblöđrótt basalt, bólstraberg|Pillow basalt, small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_71|P-71|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-14|489894|408445|-19.20785|64.17858|425|13|Stakblöđrótt, stórdílótt basalt|Porphyritic basalt, minor vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_72|P-72|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-14|489894|408445|-19.20785|64.17858|425|15|Stakblöđrótt, stórdílótt basalt|Porphyritic basalt, minor vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_73|P-73|Pálsson et al., 1984|Pálsson et al., 1972|12.6.1970|Borehole|Hrauneyjar HP-14|489894|408445|-19.20785|64.17858|425|15|Stakblöđrótt, stórdílótt basalt|Porphyritic basalt, minor vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_74|P-74|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1970|Borehole|Hrauneyjar HP-20|491905|411882|-19.16668|64.20947|436|10|Smáblöđrótt basalt, bólstraberg| Pillow basalt with small vesicles |Lava flow|Porphyritic basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.210|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_75|P-75|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1970|Borehole|Hrauneyjar HP-20|491905|411882|-19.16668|64.20947|436|11|Smáblöđrótt basalt, bólstraberg| Pillow basalt with small vesicles |Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_76|P-76|Pálsson et al., 1984|Pálsson et al., 1972|6.8.1970|Borehole|Hrauneyjar HP-22|487652|410167|-19.25412|64.19397|377|5|Smáblöđrótt basalt, kubbaberg|Entablature basalt with small vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.045|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_77|P-77|Pálsson et al., 1984|Pálsson et al., 1972|6.8.1970|Borehole|Hrauneyjar HP-22|487652|410167|-19.25412|64.19397|377|13|Smáblöđrótt basalt, kubbaberg|Entablature basalt with small vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_78|P-78|Pálsson et al., 1984|Pálsson et al., 1972|6.8.1970|Borehole|Hrauneyjar HP-22|487652|410167|-19.25412|64.19397|377|16|Smáblöđrótt basalt|Basalt with small vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.165|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.075|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_79|P-79|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-38|489394|408362|-19.21813|64.17782|421|3|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_80|P-80|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-38|489394|408362|-19.21813|64.17782|421|11|Fremur blöđrulítiđ stórdílótt basalt|Porphyritic basalt with low vesicularity|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.095|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_81|P-81|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 11|347971|384246|-22.09998|63.92823|290||Brúnleitt túff|Brown-colored tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_82|P-82|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 12|347971|384246|-22.09998|63.92823|290||Ljósbrúnt túff|Light-brown tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.420|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.430|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_83|P-83|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 13|347971|384246|-22.09998|63.92823|290||Fíngert, grćnleitt ţursaberg|Fine, green-colored agglomeritic  breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.450|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.430|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_84|P-84|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 14|347971|384246|-22.09998|63.92823|290||Ljósbrúnt túff|Light-brown tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.79|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.440|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.440|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_85|P-85|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 15|347971|384246|-22.09998|63.92823|290||Blöđrulítid, fínkornótt basalt međ holufyllingum, gangberg|Fine-grained basaltic dyke with low vesicularity and filled vesicles|Basaltic intrusion|Fine-medium grained basaltic intrusion|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_86|P-86|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 16|347971|384246|-22.09998|63.92823|290||Brúnt túff međ kalsíteitlum|Brown tuff with calcite precipitates|Hyaloclastite|Hyaloclastite tuff|Altered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.230|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_87|P-87|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 17|347971|384246|-22.09998|63.92823|290||Blöđrulaust, fínkornótt basalt úr gangi|Vesicle-free fine-grained basaltic dyke|Basaltic intrusion|Fine-medium grained basaltic intrusion|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.160|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_88|P-88|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 18|347971|384246|-22.09998|63.92823|290||Gulleitt túff|Yellow tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.64|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.370|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.370|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_89|P-89|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 19|347971|384246|-22.09998|63.92823|290||Brúnleitt túff|Brown tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.77|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.450|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.450|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_90|P-90|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 20|347971|384246|-22.09998|63.92823|290||Rautt, fíngert ţursaberg|Red, fine-grained breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.490|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_91|P-91|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 21|347971|384246|-22.09998|63.92823|290||Ummyndađ basaltgjall|Altered basalt scoria|Basaltic intrusion|Fine-medium grained basaltic intrusion|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_92|P-92|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 22|347971|384246|-22.09998|63.92823|290||Rauđleitt túff|Oxidized tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.540|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.530|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_93|P-93|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 23|347971|384246|-22.09998|63.92823|290||Brúnleitt ţursaberg|Brown-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.480|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_94|P-94|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 24|347971|384246|-22.09998|63.92823|290||Fíngert, dökkbrúngrćnleitt ţursaberg|Fine, dark brown-green agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.86|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.490|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.490|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_95|P-95|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 25|347971|384246|-22.09998|63.92823|290||Brúnleitt túff|Brown colored tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.79|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.510|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.490|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_96|P-96|Pálsson et al., 1984|Pálsson et al., 1972|4.5.1971|Borehole|Krísuvíkursvćđi H-5 (KR-05)|351907|381525|-22.01720|63.90557|142|428|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_97|P-97|Pálsson et al., 1984|Pálsson et al., 1972|4.5.1971|Borehole|Krísuvíkursvćđi H-5 (KR-05)|351907|381525|-22.01720|63.90557|142|670|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|2.80|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_98|P-98|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|3|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_99|P-99|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|5|Fremur stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_100|P-100|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|11|Nćrri blöđrulaust, stórdílótt basalt|Porphyritic basalt with almost no vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_101|P-101|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|18|Blöđrulítiđ, dílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_102|P-102|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|19|Fremur smáblöđrótt, dílótt basalt|Porphyritic basalt with small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_103|P-103|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|21|Blöđrulítiđ, dílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_104|P-104|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|23|Blöđrulítiđ, dílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_105|P-105|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|29|Nćrri blöđrulaust, dílótt basalt|Porphyritic basalt with almost no vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_106|P-106|Pálsson et al., 1984|Pálsson et al., 1972|1.6.1970|Borehole|Hrauneyjar HP-15|488914|407663|-19.22796|64.17153|440|35|Fremur blöđrulítiđ, dílótt basalt|Porphyritic basalt with minor  vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.075|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_107|P-107|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Hlíđarbrekkur Vestmannaeyjum H-1 (HB-1)|435941|327280|-20.28348|63.44490|95|782|Túffkennt ţursaberg|Tuffaceous agglomerate|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.173|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.143|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_108|P-108|Pálsson et al., 1984|Pálsson et al., 1972|12.8.1970|Borehole|Hrauneyjar HP-23|488849|410059|-19.22948|64.19303|465|30|Smáblöđrótt basalt, bólstraberg|Pillow basalt with small vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_109|P-109|Pálsson et al., 1984|Pálsson et al., 1972|12.8.1970|Borehole|Hrauneyjar HP-24|488849|410059|-19.22757|64.19112|457|12|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.270|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_110|P-110|Pálsson et al., 1984|Pálsson et al., 1972|12.8.1970|Borehole|Hrauneyjar HP-24|488849|410059|-19.22757|64.19112|457|16|Ţursaberg|Agglomerate|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.310|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.280|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_111|P-111|Pálsson et al., 1984|Pálsson et al., 1972|23.8.1970|Borehole|Hrauneyjar HP-27|488444|410959|-19.23787|64.20108|355|14|Jökulberg ađ mestu úr sandi og mélu|Tillite mostly sand and clay|Sediment|Sediment|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_112|P-112|Pálsson et al., 1984|Pálsson et al., 1972|23.8.1970|Borehole|Hrauneyjar HP-27|488444|410959|-19.23787|64.20108|355|18|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.365|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.365|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_113|P-113|Pálsson et al., 1984|Pálsson et al., 1972|23.8.1970|Borehole|Hrauneyjar HP-27|488444|410959|-19.23787|64.20108|355|20|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.315|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.290|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_114|P-114|Pálsson et al., 1984|Pálsson et al., 1972|28.8.1970|Borehole|Hrauneyjar HP-28|488448|411116|-19.23782|64.23786|375|17|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.340|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_115|P-115|Pálsson et al., 1984|Pálsson et al., 1972|28.8.1970|Borehole|Hrauneyjar HP-28|488448|411116|-19.23782|64.23786|375|19|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.270|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.240|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_116|P-116|Pálsson et al., 1984|Pálsson et al., 1972|17.9.1970|Borehole|Hrauneyjar HP-30|488542|410547|-19.23583|64.19740|395|14|Jökulberg ađ mestu úr sandi og mélu|Tillite mostly sand and clay|Sediment|Sediment|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.310|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.300|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_117|P-117|Pálsson et al., 1984|Pálsson et al., 1972|3.9.1970|Borehole|Hrauneyjar HP-31|488499|410891|-19.23673|64.20048|360|10|Jökulberg ađ mestu úr sandi og mélu|Tillite mostly sand and clay|Sediment|Sediment|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_118|P-118|Pálsson et al., 1984|Pálsson et al., 1972|3.9.1970|Borehole|Hrauneyjar HP-31|488499|410891|-19.23673|64.20048|360|13|Jökulberg ađ mestu úr sandi og mélu|Tillite mostly sand and clay|Sediment|Sediment|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.350|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_119|P-119|Pálsson et al., 1984|Pálsson et al., 1972|3.9.1970|Borehole|Hrauneyjar HP-31|488499|410891|-19.23673|64.20048|360|16|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.285|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_120|P-120|Pálsson et al., 1984|Pálsson et al., 1972|3.9.1970|Borehole|Hrauneyjar HP-31|488499|410891|-19.23673|64.20048|360|20|Jökulberg ađ mestu úr sandi og mélu|Tillite mostly sand and clay|Sediment|Sediment|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.280|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_121|P-121|Pálsson et al., 1984|Pálsson et al., 1972|3.9.1970|Borehole|Hrauneyjar HP-31|488499|410891|-19.23673|64.20048|360|24|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.260|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_122|P-122|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|3|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_123|P-123|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|6|Nćrri blöđrulaust, stórdílótt basalt|Porphyritic basalt with almost no vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_124|P-124|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|7|Međalblöđrótt, stórdílótt basalt|Porphyritic basalt with medium-sized vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_125|P-125|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|10|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_126|P-126|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|11|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.280|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_127|P-127|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|11|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_128|P-128|Pálsson et al., 1984|Pálsson et al., 1972|15.9.1970|Borehole|Hrauneyjar HP-34|488951|409752|-19.22733|64.19028|456|13|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_129|P-129|Pálsson et al., 1984|Pálsson et al., 1972|2.10.1970|Borehole|Hrauneyjar HP-35|488994|409696|-19.22645|64.18978|449|4|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_130|P-130|Pálsson et al., 1984|Pálsson et al., 1972|2.10.1970|Borehole|Hrauneyjar HP-35|488994|409696|-19.22645|64.18978|449|6|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_131|P-131|Pálsson et al., 1984|Pálsson et al., 1972|2.10.1970|Borehole|Hrauneyjar HP-35|488994|409696|-19.22645|64.18978|449|11|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_132|P-132|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-37|489112|409333|-19.22400|64.18653|421|12|Nćrri blöđrulaust, stórdílótt basalt|Porphyritic basalt with almost no vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_133|P-133|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-37|489112|409333|-19.22400|64.18653|421|13|Nćrri blöđrulaust, stórdílótt basalt|Porphyritic basalt with almost no vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_134|P-134|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-37|489112|409333|-19.22400|64.18653|421|16|Stórblöđrótt, stórdílótt basalt|Porphyritic basalt with large vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_135|P-135|Pálsson et al., 1984|Pálsson et al., 1972|9.9.1970|Borehole|Hrauneyjar HP-37|489112|409333|-19.22400|64.18653|421|34|Mjög blöđrótt, stórdílótt basalt|Porphyritic basalt, very vesicular|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_136|P-136|Pálsson et al., 1984|Pálsson et al., 1972|19.10.1970|Borehole|Hrauneyjar HP-41|490023|407534|-19.20515|64.17042|430|4|Fremur blöđrulítiđ stórdílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_137|P-137|Pálsson et al., 1984|Pálsson et al., 1972|19.10.1970|Borehole|Hrauneyjar HP-41|490023|407534|-19.20515|64.17042|430|6|Fremur blöđrulítiđ stórdílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_138|P-138|Pálsson et al., 1984|Pálsson et al., 1972|19.10.1970|Borehole|Hrauneyjar HP-41|490023|407534|-19.20515|64.17042|430|9|Blöđrulítiđ stórdílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_139|P-139|Pálsson et al., 1984|Pálsson et al., 1972|19.10.1970|Borehole|Hrauneyjar HP-41|490023|407534|-19.20515|64.17042|430|10|Fremur blöđrulítiđ stórdílótt basalt|Porphyritic basalt with minor vesicles|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_140|P-140|Pálsson et al., 1984|Pálsson et al., 1972|19.10.1970|Borehole|Hrauneyjar HP-42|488869|409967|-19.22905|64.19222|462|6|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.275|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_141|P-141|Pálsson et al., 1984|Pálsson et al., 1972|12.8.1970|Borehole|Hrauneyjar HP-23|488849|410059|-19.22948|64.19303|465|21|Dálítiđ leirfyllt bólstraberg|Pillow lava with clay-filled vesicles|Pillow basalt|Pillow basalt|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_142|P-142|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|6|Jökulberg|Tillite|Sediment|Sediment|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.270|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_143|P-143|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|10|Fíngert jökulberg|Fine tillite|Sediment|Sediment|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.275|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_144|P-144|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|10|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.270|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.260|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_145|P-145|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|18|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_146|P-146|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|22|Jökulberg|Tillite|Sediment|Sediment|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.260|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.240|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_147|P-147|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|23|Bólstraberg međ leirfyllingum|Pillow basalt with clay fillings|Pillow basalt|Pillow basalt|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_148|P-148|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|24|Bólstraberg međ leirfyllingum|Pillow basalt with clay fillings|Pillow basalt|Pillow basalt|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.240|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_149|P-149|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|26|Bólstraberg međ leirfyllingum|Pillow basalt with clay fillings|Pillow basalt|Pillow basalt|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.250|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_150|P-150|Pálsson et al., 1984|Pálsson et al., 1972|10.9.1970|Borehole|Hrauneyjar HP-46|488438|410858|-19.23798|64.20018|360|28|Bólstraberg međ leirfyllingum|Pillow basalt with clay fillings|Pillow basalt|Pillow basalt|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.230|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_151|P-151|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|3|Stórblöđrótt, stórdílótt basalt, THh|Porphyritic basalt with large vesicles|Pillow basalt|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_152|P-152|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|5|Blöđrótt, stórdílótt basalt, THh|Vesicular porphyritic basalt|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.160|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_153|P-153|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|9|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_154|P-154|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|11|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_155|P-155|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|15|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_156|P-156|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|22|Stórblöđrótt, stórdílótt basalt, THh|Porphyritic basalt with large vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_157|P-157|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|24|Stórblöđrótt, stórdílótt basalt, THh|Porphyritic basalt with large vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_158|P-158|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|26|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_159|P-159|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|30|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_160|P-160|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|31|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.650|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_161|P-161|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|39|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_162|P-162|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|43|Blöđrulítiđ, stórdílótt basalt, THh|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_163|P-163|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|47|Tćplega međalblöđrótt, stórdílótt basalt, THf|Porphyritic basalt with medium vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_164|P-164|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|52|Stórblöđrótt, stórdílótt basalt, THc|Porphyritic basalt with large vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_165|P-165|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|54|Fremur blöđrulítiđ, stórdílótt basalt, THc|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_166|P-166|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|58|Blöđrulítiđ, stórdílótt basalt, THc|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.115|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.095|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_167|P-167|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|60|Tćplega međalblöđrótt, stórdílótt basalt, THf|Porphyritic basalt with medium vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_168|P-168|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|67|Blöđrulítiđ, stórdílótt basalt, THc|Porphyritic basalt with minor vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_169|P-169|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|69|Međalblöđrótt, stórdílótt basalt, THc|Porphyritic basalt with medium-size vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.115|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.105|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_170|P-170|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|71|Fremur smáblöđrótt, stórdílótt basalt, THc|Porphyritic basalt with small vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_171|P-171|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|74|Mjög blöđrótt, stórdílótt basalt, THc|Very vesicular porphyritic basalt, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.250|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_172|P-172|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|77|Töluvert blöđrótt, dílótt basalt, THc|Porphyritic basalt with medium vesicularity, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.260|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_173|P-173|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|78|Međalblöđrótt, dílótt basalt, Tha eđa THb|Porphyritic basalt with medium vesicularity, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_174|P-174|Pálsson et al., 1984|Pálsson et al., 1972|29.7.1970|Borehole|Sigalda E-8|494660|405861|-19.10975|64.15552|494|79|Fremur smáblöđrótt, dílótt basalt, Tha eđa THb|Porphyritic basalt with small vesicles, from Tugnárhraun|Lava flow|Porphyritic basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_175|P-175|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 26|391294|393644|-21.22442|64.02882|189||Mjög fínkornótt, ólivíndílótt basalt|Very fine-grained olivine porphyritic basalt|Lava flow|Porphyritic basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_176|P-176|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 27|391294|393644|-21.22442|64.02882|189||Grćnt túff međ miklu af pýríti|Green tuff with abundant pyrite|Hyaloclastite|Hyaloclastite tuff|Altered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.320|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.310|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_177|P-177|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 28|391294|393644|-21.22442|64.02882|189||Ljóst molaberg|Light coloured sedimentary rock|Sediment|Sediment|Unaltered|2.72|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_178|P-178|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 29|391294|393644|-21.22442|64.02882|189||Brúngrćnleitt túff|Brown-green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.91|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_179|P-179|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 30|391294|393644|-21.22442|64.02882|189||Ljósgrátt, ummyndađ berg|Light-gray altered rock|Hyaloclastite|Hyaloclastite tuff|Altered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.210|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_180|P-180|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 31|391294|393644|-21.22442|64.02882|189||Grágrćnt, ummyndađ bólstraberg|Grey-green altered pillow basalt|Pillow basalt|Pillow basalt|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_181|P-181|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 32|391294|393644|-21.22442|64.02882|189||Dökkbrúnt bólstraberg|Dark-brown pillow basalt|Pillow basalt|Pillow basalt|Unaltered|2.87|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_182|P-182|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 33|391294|393644|-21.22442|64.02882|189||Ljósgrćnt, ummyndađ bólstraberg|Light-green altered pillow basalt|Pillow basalt|Pillow basalt|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.340|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.300|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_183|P-183|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 34|391294|393644|-21.22442|64.02882|189||Brúnleitt ţursaberg|Brown-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.81|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.380|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.360|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_184|P-184|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 35|391294|393644|-21.22442|64.02882|189||Ljósbrúngrćnleitt túff|Light-brown-green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.430|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.390|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_185|P-185|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 36|391294|393644|-21.22442|64.02882|189||Blöđrulaust basalt|Vesicle-free basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.450|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_186|P-186|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 37|391294|393644|-21.22442|64.02882|189||Dökkbrúnleitt túff|Dark-brown tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.340|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_187|P-187|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Slaga í Sveifluhálsi á Reykjanesskaga|347589|378282|-22.10179|63.87463|283||Rautt ţursaberg|Red agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.90|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.490|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.470|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_188|P-188|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvćđi H-6|348640|386389|-22.08850|63.94772|145|412|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_189|P-189|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvćđi H-6|348640|386389|-22.08850|63.94772|145|413|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_190|P-190|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvćđi H-6|348640|386389|-22.08850|63.94772|145|625|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_191|P-191|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvćđi H-6|348640|386389|-22.08850|63.94772|145|821|Ummyndađ basalt|Altered basalt|Lava flow|Fine-medium grained basaltic lava|Altered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_192|P-192|Pálsson et al., 1984|Pálsson et al., 1972|24.9.1962|Borehole|Ártún H-38|361791|405231|-21.83777|64.12208|16|300|Fíngert ţursaberg|Fine-grained breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.370|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.340|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_193|P-193|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Njarđvíkurheiđi|327604|390687|-22.52179|63.97636|3|210|Dílalaust, blöđrótt grágrýti|Vesicular aphyric olivine tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.160|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_194|P-194|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Njarđvíkurheiđi|327604|390687|-22.52179|63.97636|3|497|Mjög fínkornótt, blöđrulaust basalt|Very fine-grained vesicle-free basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_195|P-195|Pálsson et al., 1984|Pálsson et al., 1972|18.8.1971|Borehole|Krísuvíkursvćđi H-7|348336|383153|-22.09147|63.91860|200|155|Blöđrulaust basalt međ stórum plagíoklas- og ólivíndílum|Compact plagioclase and olivine porphyritic basalt|Lava flow|Porphyritic basaltic lava|Unaltered|2.95|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_196|P-196|Pálsson et al., 1984|Pálsson et al., 1972|18.8.1971|Borehole|Krísuvíkursvćđi H-7|348336|383153|-22.09147|63.91860|200|186|Dílalaust, mjög blöđrulítiđ basalt|Aphyric relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_197|P-197|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvćđi H-8|349112|381938|-22.07447|63.90805|264|377|Brúnleitt, ummyndađ basalt|Brown-colored altered basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_198|P-198|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvćđi H-8|349112|381938|-22.07447|63.90805|264|378|Brúnleitt, ummyndađ basalt|Brown-colored altered basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_199|P-199|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvćđi H-8|349112|381938|-22.07447|63.90805|264|736|Grćnleitt berg međ hvítum dilum|Green-colored rock with white minerals |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_200|P-200|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvćđi H-8|349112|381938|-22.07447|63.90805|264|930|Grćnleitt berg|Green-colored rock|Hyaloclastite|Hyaloclastite tuff|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_201|P-201|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Hjalli í Ölfusi|||||||Olivínbasalt|Olivine tholeiite basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_202|P-202|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Hjalli í Ölfusi|||||||Basalt|Basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_203|P-203|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöđrótt basalt međ strjálum plagíóklasdílum|Vesicular basalt sparsely plagioclase porphyritic|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.90|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_204|P-204|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Stórblöđrótt basalt međ holufyllingum|Basalt with large vesicles containing amygdales|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.87|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_205|P-205|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Misblöđrótt basalt međ strjálum plagíóklasdílum|Basalt with heterogeneous vesicularity  and sparesly plagioclase phenocrysts|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_206|P-206|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Smáblöđrótt basalt|Basalt with small vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_207|P-207|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöđrótt basalt|Vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_208|P-208|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöđrótt, gjallkennt basalt|Vesicular, scoriaceous basalt|Lava flow|Flow-top breccia|Unaltered|2.42|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_209|P-209|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöđrulítiđ basalt međ smáum plagíóklasdílum|Relatively compact basalt, with small plagioclase phenocrysts|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_210|P-210|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöđrulítiđ basalt međ smáum plagíóklasdílum|Relatively compact basalt, with small plagioclase phenocrysts|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_211|P-211|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Stakblöđrótt basalt međ smáum plagíóklasdílum|Relatively compact basalt with small plagioclase microphenocrysts|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_213|P-213|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niđri viđ sjó, IBF-4-810-5|||||||Grćnt, hart túff međ strjálum basaltmolum|Green hardened tuff with occasional basalt fragments|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.190|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_214|P-214|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niđri viđ sjó, IBF-4-810-6|||||||Grćnt, hart túff međ strjálum basaltmolum|Green hardened tuff with occasional basalt fragments|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.230|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_215|P-215|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niđri viđ sjó, IBF-4-810-7|||||||Grćnt, hart túff međ strjálum basaltmolum|Green hardened tuff with occasional basalt fragments|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.210|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.190|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_216|P-216|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Leiđhamar viđ Kollafjörđ undir Háspennulínu, IBF-4-810-8|||||||Grćnt, hart túff međ strjálum basalt- og leirmolum|Green hardened tuff with occasional basalt and clay fragments|Hyaloclastite|Hyaloclastite tuff|Altered|2.83|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_217|P-217|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan viđ Ártún, IBF-2-137-2|||||||Dílótt ţóleiít úr hrauni|Porphyritic tholeiite lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_218|P-218|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Lokufjall, IBF-2-197-1|||||||Ţóleiít úr hrauni|Tholeiitic lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_219|P-219|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Lokufjall viđ Tíđaskarđ, IBF-2-227-1|||||||Íslandít úr gangi|Icelandite dyke|Intermediate intrusion|Diorite|Unaltered|2.72|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_220|P-220|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestanvert Kerlingagil, IBF-1-166-1|||||||Dílótt ţóleiít úr gígtappa|Porphyritic tholeiite from crater plug|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_221|P-221|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, suđvestan Tindstađahnúkur, IBF-1-46-5|||||||Ţóleiít úr gígtappa|Tholeiite from crater plug|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_222|P-222|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, áin austan viđ bćinn Flekkudal, IBF-1-97-3|||||||Ţóleiít úr bólstra|Tholeiite from pillow|Pillow basalt|Pillow basalt|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_223|P-223|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestan viđ Kerhólakamb, IBF-2-28-1|||||||Dílótt ţóleiít úr gígtappa|Porphyritic tholeiite from crater plug|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_224|P-224|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestan í Skálatindi, IBF-1-246-1|||||||Fínkornótt ólvivínţóleiít úr hrauni|Fine-grained olivine tholeiite  lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_225|P-225|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vesturhlíđ Eilísfdals, IBF-1-226-1|||||||Fínkornótt ólvivínţóleiít úr hrauni|Fine-grained olivine tholeiite lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_226|P-226|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norđan í ţórnýjartindi, IBF-1-216-3|||||||Ólivínţóleiít úr hrauni|Olivine tholeiitic lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_227|P-227|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Ţverárdalur, IBF-1-99-1|||||||Ţóleiít úr hrauni|Tholeiitic lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_228|P-228|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Bláhnúkur, IBF-1-98-2|||||||Basaltandesít úr gígtappa|Basalt andesite crater plug|Intermediate volcanic|Basaltic andesite|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_229|P-229|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norđan viđ Leirvogsá, suđvestan Tröllafoss, IBF-259-7|||||||Ţóleiítdólerít úr stuđluđu innskoti|Tholeiitic dolerite from columnar intrusion|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_230|P-230|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sunnan í stardalshnúk, IBF-249-4|||||||Ólivínţóleiítdólerít úr stuđli|Olivine tholeiitic dolerite column|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_231|P-231|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norđan í ţórnýjartindi, IBF-1-216-2|||||||Fínkornótt ţóleiít úr hrauni|Fine-grained tholeiite lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.10|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_232|P-232|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Múli, IBF-1-229-6|||||||Líparít, blöđrur ađ nokkru kvarsfylltar|Rhyolite, vesicles partly filled with quartz|Silicic intrusion|Rhyolite dyke|Unaltered|2.61|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_233|P-233|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Múli, IBF-1-229-7|||||||Íslandít, seólítar í holum|Icelandite, zeolites in vesicles|Intermediate volcanic|Icelandite (andesite)|Unaltered|2.73|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_234|P-234|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, í gili sunnan viđ Trönu, IBF-1-76-1|||||||Fínkornótt, dílótt basaltandesít|Fine-grained porphyritic basalt andesite|Intermediate volcanic|Basaltic andesite|Unaltered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_235|P-235|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan í Kistufelli, IBF-1-128-1|||||||Dílótt ţóleiít|Porphyritic tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_236|P-236|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grímmannsfell, Austan í Dalhólum, IBF-2-228-2|||||||Fínkornótt ólivínţóleiít úr gígtappa|Fine-grained olivine tholeiite crater plug|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_237|P-237|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Viđ Leirvogsá, vestan viđ Tröllafoss, IBF-249-9|||||||Líparít úr gangi|Rhyolitic dyke|Silicic intrusion|Rhyolite dyke|Unaltered|2.62|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.220|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.190|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_238|P-238|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Kerlinagil, IBF-4-2611-1|||||||Ţóleiít úr miđju hraunlagi|Tholeiite from the middle of a lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_240|P-240|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Kerlinagil, IBF-4-2611-3|||||||Ţóleiít úr miđju hraunlagi|Tholeiite from the middle of a lava|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_244|P-244|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Melafjall, IBF-4-46-9|||||||Blöđrótt, straumlögótt ţóleiít|Vesicular, flow-banded tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_245|P-245|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norđurhlíđ Melafjalls, IBF-4-46-10|||||||Ólivínţóleiít|Olivine tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_246|P-246|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan Tíđaskarđs, viđ mynni Blikdals, IBF-4-46-12|||||||Ólívínţóleiít|Olivine tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_247|P-247|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sunnan Tindstađa. IBF-1-296-1|||||||Dílótt ţóleiít úr hrauni|Porphyritic tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_248|P-248|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norđurhlíđ Sneiđa, IBF-5-204-2|||||||Stórdílótt ţóleiít úr hrauni|Porphyritic tholeiite, large phenocrysts|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_249|P-249|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sneiđar, IBF-5-204-1|||||||Dílótt ólivínţóleiít úr hrauni|Porphyritic olivine tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_250|P-250|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, suđvestan viđ Kerhólakamb, IBF-2-28-1|||||||Dílótt ţóleiít úr hrauni|Porphyritic tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_251|P-251|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norđaustan í ţórnýjartindi, IBF-1-216-1|||||||Dílótt ólívínţóleiít úr hrauni|Porphyritic olivine tholeiite|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_252|P-252|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Ţverárkotsháls, IBF-39-1|||||||Dílótt ólivínţóleiít úr hrauni|Porphyritic olivine tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_253|P-253|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Nónbunga, IBF-1-87-1|||||||Ólivínţóleiít úr hrauni|Olivine tholeiite lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.11|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.150|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_254|P-254|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norđan viđ Helgafell í Mosfellssveit, IBF-1-259-7|||||||Ţóleiít úr hrauni|Tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_255|P-255|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, austurhlíđ Trönu, IBF-1-37-2|||||||Dílótt ţóleiít úr hrauni|Porphyritic tholeiite lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.09|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.800|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_256|P-256|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stardalur, IBF-1-139-1|||||||Fínkornótt íslandít úr hrauni|Fine-grained icelandite lava|Intermediate volcanic|Icelandite (andesite)|Unaltered|2.60|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.100|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_257|P-257|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Krafla H-1 (K-2, KG-2)|602736|581470|-16.76184|65.72769|571|540|Nćr eingöngu basalt, ţursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_258|P-258|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur viđ Hjörleifshöfđa|324217|511259|-18.77461|63.42308|19||Ţursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.60|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.230|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_259|P-259|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur viđ Hjörleifshöfđa|324217|511259|-18.77461|63.42308|19||Gjallkennt basalt eđa andesít|Scoriaceous basalt or andesite|Intermediate volcanic|Icelandite (andesite)|Unaltered|2.72|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.370|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_260|P-260|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur viđ Hjörleifshöfđa|324217|511259|-18.77461|63.42308|19||Grófkornótt túff|Coarse-grained tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.62|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.350|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_261|P-261|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Straumlögótt andesít úr bólstra|Flow-banded andesite pillow|Intermediate volcanic|Icelandite (andesite)|Unaltered|2.57|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_262|P-262|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Hrafntinna úr bólstra, IBF-5-238-2|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.46|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_263|P-263|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll|458923|488525|-19.23995|64.63134|1162||Hraftinna, IBF-5-188-1|Obsidian|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.45|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_264|P-264|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Geldingsadalsfjall í Gnúpverjahreppi|394901|438355|-20.26216|64.05173|107||Blöđrótt, nokkuđ holufyllt basalt úr gangi, IBF-5-248-2|Vesicular basalt dyke with filled amygdales |Basaltic intrusion|Fine-medium grained basaltic intrusion|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.240|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_265|P-265|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll|458923|488525|-19.23995|64.63134|1162||Blöđrótt líparít úr bólstra, IBF-5-188-1|Vesicular rhyolite pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.45|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.220|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_266|P-266|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Blöđrótt hrafntinna, IBF-5-238-4|Vesicular obsidian|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.54|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_267|P-267|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Líparít úr miđjum bólstra, IBF-5-228-2|Rhyolite from the middle of a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.52|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.230|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_268|P-268|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Straumlögótt líparít úr bólstra, IBF-5-228-4|Flow-banded rhyolite pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.52|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_269|P-269|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Víkurkennt líparít milli bólstra, IBF-5-238-3|Pumice-like rhyolite between pillows|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.39|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.265|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_270|P-270|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár viđ Brúna|407518|493284|-19.13810|64.17036|432||Basalt, IBF-5-248-1|Basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.06|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_271|P-271|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kálfstindar|||||||Basalt, IBF-5-258-1|Basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.170|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_272|P-272|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll, Fremri-Árskarđsá|458923|488525|-19.23995|64.63134|1162||Basaltandesít úr miđjum bólstra, IBF-5-208-1|Basalt andesite from the middle of the pillow|Intermediate volcanic|Basaltic andesite|Unaltered|2.81|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.290|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_273|P-273|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll, Norđausturhlíđ Lođmundar|458923|488525|-19.23995|64.63134|1162||Mjög blöđrótt andesít, 99.9% syrtiđ (opaque), IBF-5-198-6|Very vesicular andesite, microcrystalline|Intermediate volcanic|Icelandite (andesite)|Unaltered|2.69|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.420|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.350|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_274|P-274|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Geldingsadalsfjall í Gnúpverjahreppi|394901|438355|-20.26216|64.05173|107||Líparít úr innskoti, IBF-5-248-5|Rhyolitic intrusion|Silicic intrusion|Rhyolite dyke|Unaltered|2.53|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_275|P-275|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll|458923|488525|-19.23995|64.63134|1162||Dasít, IBF-5-178-9|Dacite|Intermediate volcanic|Dacite|Unaltered|2.79|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_276|P-276|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Selfjall suđvestan geitár|435344|385757|-21.36935|64.40082|388||Basaltandesít|Basaltic andesite|Intermediate volcanic|Basaltic andesite|Unaltered|2.88|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.400|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_277|P-277|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll|458923|488525|-19.23995|64.63134|1162||Líparítvikur, IBF-5-178-2|Rhyolite pumice|Silicic volcanic|Rhyolite lava|Unaltered|2.39|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.570|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.530|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_278|P-278|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Brimnes Norđan Kollafjarđar, IBF-5-3010-1|||||||Dílótt ţóleiít úr hrauni|Porphyritic tholeiitic lava|Lava flow|Porphyritic basaltic lava|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_279|P-279|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Trönudalur, IBF-5-268-1|||||||Basaltandesít úr bólstra|Basalt andesite  pillow|Intermediate volcanic|Basaltic andesite|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.600|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_280|P-280|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Trönudalur, IBF-5-268-4|||||||Basaltandesít úr bólstra|Basalt andesite  pillow|Intermediate volcanic|Basaltic andesite|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.060|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_281|P-281|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kálfstindar|||||||Blöđrótt, glerkennt basalt yst úr bólstra, IBF-5-258-2|Vesicular, vitreous basalt at the outer boundary of a pillow|Pillow basalt|Pillow basalt|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.290|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_282|P-282 - P-285|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Krafla H-5 (K-2, KG-2)|602736|581470|-16.76184|65.72769|571|790|Túffkennt, mjög ummyndađ ţursaberg|Tuffaceous very altered agglomerate breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.70|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.155|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_286|P-286 - P-287|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Krafla H-5 (K-2, KG-2)|602736|581470|-16.76184|65.72769|571|790|Ţétt basalt|Compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.87|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.450|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.035|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_288|P-288|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-1 (FV-1)|686755|506955|-15.03688|65.06161|603|44|Fínkornótt, blöđrulítiđ basalt|Fine-grained, relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_289|P-289|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-1 (FV-1)|686755|506955|-15.03688|65.06161|603|101|Blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_290|P-290|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-1 (FV-1)|686755|506955|-15.03688|65.06161|603|152|Fínkornótt, blöđrulaust basalt|Fine grained compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.02|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_291|P-291|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-1 (FV-1)|686755|506955|-15.03688|65.06161|603|208|Fínkornótt, blöđrulítiđ basalt|Fine-grained relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_292|P-292|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|9|Fínkornótt, blöđrulítiđ basalt|Fine-grained relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_293|P-293|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|39|Rauđbrúnt, fínkornótt ţursaberg|Red-brown fine grained agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.56|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.240|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_294|P-294|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|39|Rauđbrúnn sandsteinn|Red-brown reworked tuff sediment|Hyaloclastite|Hyaloclastite sediment|Unaltered|2.46|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.210|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_295|P-295|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|142|Stórblöđrótt, töluvert holufyllt basalt|Basalt with numerous, large, partially filled vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.82|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.200|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_296|P-296|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|173| Fínkornótt, böđrulaust basalt|Fine-grained compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.020|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_297|P-297|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-3 (FV-3)|686051|508455|-15.04979|65.07546|640|14| Blöđrulítid, gráleitt, smádílótt basalt|Grey sparesly vesiculated microporhyritic basalt|Lava flow|Porphyritic basaltic lava|Unaltered|2.86|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_298|P-298|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Mjóifjörđur viđ Ísafjarđardjúp|603169|338429|-22.54422|65.88470|139||Stakblöđrótt basalt|Sparesly vesiculated basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.91|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_299|P-299|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Ísafjörđur|625860|314147|-23.10776|66.07464|5||Smádílótt, nćrri blöđrulaust basalt|Microporphyritic relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_300|P-300|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Skötufjörđur|609557|327174|-22.79893|65.93603|2||Grátt, dílótt, blörulaust basalt|Grey, porphyritic, non-vesicular basalt|Lava flow|Porphyritic basaltic lava|Unaltered|2.98|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_301|P-301|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Álftafjörđur viđ Ísafjarđardjúp|615922|317512|-23.01966|65.98764|12||Gráleitt basalt međ fáum holufylltum blöđrum|Grey basalt with a few filled vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.90|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_302|P-302|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Hestfjörđur|613111|324581|-22.86056|65.96643|82||Grátt, dílótt, blörulítiđ basalt|Grey porphyritic relatively compact basalt|Lava flow|Porphyritic basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)||Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_303|P-303|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norđvesturhlíđ Bláhnúks (Laugahnúks) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Blöđrulítiđ líparít úr gangi eđa tappa, IBF-6-29-2|Rhyolite dike or feeder with minor vesicles|Silicic intrusion|Rhyolite dyke|Unaltered|2.51|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.120|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_304|P-304|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíđ Bláhnúks (Laugahnúks) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miđjum bolstra, IBF-6-29-5|Rhyolite from the middle of pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.49|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_305|P-305|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíđ Bláhnúks (Laugahnúks) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miđjum bolstra, IBF-6-29-6|Rhyolite from the middle of pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.51|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.150|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_306|P-306|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíđ Bláhnúks (Laugahnúks) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Hrafntinna úr bolstra, IBF-6-29-7|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.46|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.700|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_307|P-307|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Hrafntinna úr bolstra, IBF-6-29-9|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.52|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.260|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.230|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_308|P-308|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Víkurkennt líparít úr bolstra, IBF-6-29-10|Pumaceous rhyolite from a pilloe|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.57|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.330|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.320|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_309|P-309|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Hrafntinna úr bolstra, IBF-6-29-13|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.45|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_310|P-310|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Hraftinna úr bólstra, IBF-6-29-14|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.51|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_311|P-311|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Vikurkennt basalt úr bólstra, IBF-6-29-15|Pumaceous basalt from pillow|Pillow basalt|Pillow basalt|Unaltered|2.54|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_312|P-312|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Líparít úr miđjum bólstra, IBF-6-29-16|Rhyolite from the middle of a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.48|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_313|P-313|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Víkurkennt líparít úr bolstra, IBF-6-29-12|Pumaceous rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.56|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.270|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_314|P-314|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stapafell|||||||Basalt úr miđjum bólstra, IBF-6-318-9|Central part of a basalt pillow|Pillow basalt|Pillow basalt|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.160|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_315|P-315|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stapafell|||||||Basalt ofarlega úr bólstra, IBF-6-318-10|Basalt from the top of a pillow|Pillow basalt|Pillow basalt|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.340|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.230|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_316|P-316|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stapafell|||||||Basalt neđarlega úr bólstra, IBF-6-318-8|Basalt lower part of pillow|Pillow basalt|Pillow basalt|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.260|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_317|P-317|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miđjum bolstra, IBF-6-29-11|Rhyolite from the middle of a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.48|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.230|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.180|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_318|P-318|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíđ Bláhnúks (Laugahnúks) viđ Landmannalaugar|386645|496333|-19.07489|63.98317|673||Hálfvikurkennt líparít úr bólstra, IBF-6-29-4|Rhyolite from pumaceous part of pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.51|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_319|P-319|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöđrótt hrafntinna úr bólstra, IBF-6-49-1|Vesicular obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.45|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_320|P-320|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöđrulaus hrafntinna úr bólstra, IBF-6-49-2|Vesicle-free obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.49|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.900|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.030|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_321|P-321|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöđrótt, straumlögótt líparít úr bólstra, IBF-6-49-3|Vesicular flow lineated rhyolite within a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.62|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.280|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.170|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_322|P-322|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöđrótt, straumlögótt líparít úr bólstra, IBF-6-49-4|Vesicular flow lineated rhyolite within a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.59|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_323|P-323|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Blöđrulaus hrafntinna úr bólstra, IBF-6-49-7|Compact obsidian from a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.44|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.200|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.010|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_324|P-324|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grćnagil|386600|496920|-19.06290|63.98277|669||Líparít, ekki straumlögótt, úr bólstra, IBF-6-49-8|Rhyolite, not flow-banded, from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.59|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.140|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_325|P-325|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Stuđlađ líparít úr bólstra|Entablature rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.48|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.210|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_326|P-326|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Mosfell í Mosfellssveit í Gili upp af Kirkjunni, IBF-6-59-1|||||||Basalt úr miđjum bólstra|Basalt from the middle of a pillow|Pillow basalt|Pillow basalt|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_327|P-327|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár viđ Brúna|407518|493284|-19.13810|64.17036|432||Basalt úr miđjum bólstra, IBF-6-49-11|Basalt from middle of a pillow|Pillow basalt|Pillow basalt|Unaltered|3.08|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.110|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.050|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_328|P-328|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Straumlögótt líparít úr bólstra, IBF-6-49-9|Flow-banded rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.57|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_331|P-331|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár viđ Brúna|407518|493284|-19.13810|64.17036|432||Basalt úr miđjum bólstra, IBF-6-49-11|Basalt from middle of a pillow|Pillow basalt|Pillow basalt|Unaltered|3.07|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.140|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_332|P-332|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Mosfell í Mosfellssveit í Gili upp af Kirkjunni, IBF-6-59-2|||||||Basískt gler úr bólstra|Basaltic glass from pillow|Pillow basalt|Pillow basalt|Unaltered|2.86|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.120|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_333|P-333|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Líparít úr miđjum bólstra|Rhyolite from the middle of a pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.51|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_334|P-334|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Straumlögótt líparít úr bólstra|Flow-banded rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.57|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.300|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_335|P-335|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Hrafntinna úr bólstra|Obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.56|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.000|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_336|P-336|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Perlusteinn úr bólstra|Perlite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.49|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.500|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.001|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_337|P-337|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Líparít úr miđjum bólstra|Rhyolite from the middle of the pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.49|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.160|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_338|P-338|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Stuđlađ líparít úr bólstra|Columnar rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.49|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.190|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.130|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_339|P-339|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Blöđrótt hrafntinna úr bólstra|Vesicular obsidian from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.45|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.130|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_340|P-340|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Hraftinnu- og vikurkennt líparít úr bólstra|Obsidian and pumaceous rhyolite from pillow|Silicic volcanic|Rhyolite hyaloclastite|Unaltered|2.43|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.180|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.160|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_341|P-341|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Ytri-tjarnir TN-1 (YT-1)|566130|543791|-18.05068|65.59020|12|130|Ţétt ólivínţóleiít|Dense olivine tholeiite|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|0.350|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.040|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_342|P-342|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grenivík|606155|537223|-18.18183|65.94994|3||Dökkt, ólivíndílótt, stakblöđrótt basalt|Dark, olivine porphyritic basalt, slightly vesicular|Lava flow|Porphyritic basaltic lava|Unaltered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.025|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_343|P-343|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Helguvík á Rosmhvalanesi B-9|||||||Fínblöđrótt basalt|Finely vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_344|P-344|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Helguvík á Rosmhvalanesi B-10||||||18|Stórblöđrótt basalt|Coarsely vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.94|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.190|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_345|P-345|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarđvík|||||||Blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.090|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_346|P-346|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarđvík|||||||Fremur blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.76|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.070|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_347|P-347|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarđvík|||||||Mjög blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.110|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_348|P-348|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Keflavík|||||||Mjög blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.99|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.100|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_349|P-349|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sandgerđi|||||||Mjög blöđrulítiđ basalt|Relatively compact basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|||0.080|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
Palsson1984_350|P-350|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Laugardćlir ŢG-12 ||||||305|Rautt túff|Red oxidized tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|||||0.450|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)||||||||||||||||||||||||
OS-95017_G-1|G-1|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440824|-15.39058|64.42466|132||Súr gangur úr fasa 4 og ćđakerfi 3-5.|Rhyolite dyke originating from phase 4 and vein system 3-5|Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.670|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.062|He Gas pycnometry, Western Atlas Borehole Laboratories|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.95E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-2|G-2|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440828|-15.39059|64.42469|133||Breksía 3 m austan viđ sýni G-1, ţ.e. mjög sprungin basalt breksía og sprungur fylltar. Sýni tekiđ í keilugangasvarmi.|Breccia 3 m east of sample G-1. Very fractured basalt breccia with filled cracks. Sample taken from within a cone sheet swarm.|Lava flow|Flow-top breccia|Epidote-actinolite|2.67|Measured on crushed sample by Western Atlas Borehole Laboratories|0.790|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.071|He Gas pycnometry, Western Atlas Borehole Laboratories|8.78E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|8.58E-16|Measured by Western Atlas Borehole Laboratories|1.06E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-3|G-3|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440845|-15.39056|64.42484|136||Fínkornótt ţóleiítbasalt hraunlag. M.a. epidót, klórít og prenít í blöđrum. Bergid er blöđrótt, en fyllt og mjög ţétt í sér. |Fine-grained tholeiitic basalt lava. Epidote, chlorite and prehnite in vesicles. Rock is vesicular, but filled and very compact.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.370|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.006|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-4|G-4|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673793|440982|-15.39115|64.42609|155||Plagíóklasporfýr međ ţéttum grunnmassa. Allar blöđrur fylltar, sprungur áberandi og fylltar, ummyndunarbönd (e.t.v. merki um sprungur sem ekki sjást) og straumflögun.|Plagioclase porphyritic basalt with dense matrix. All vesicles filled, with prominent filled veins, wall rock alteration bands/halos (or signs of invisible cracks), flow-banding. |Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.420|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.039|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-5|G-5|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673792|440988|-15.39115|64.42614|156||Plagíóklasporfýr. Blöđróttur međ morkna ásýnd, blöđrur fylltar ađ hálfu eđa öllu leyti. Berg mjög brotiđ og straumflögótt. Sýni tekiđ viđ neđri jađar lagsins.|Plagioclase porphyritic basalt. Vesicular  and crumbly appearance, veins partially or completely filled. Rock very broken and flow-banded. Sample taken from the lower boundary of the layer. |Lava flow|Porphyritic basaltic lava|Chlorite-epidote|3.06|Measured on crushed sample by Western Atlas Borehole Laboratories|0.195|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.194|He Gas pycnometry, Western Atlas Borehole Laboratories|9.30E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.36E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-6|G-6|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673793|440997|-15.39112|64.42623|159||Sama lag og G-5 en í ţéttara bergi líklega 6 m ofar. Bergiđ er plagíóklas- dílótt, međ ţéttum grunnmassa annars á lýsingin viđ í G-5. |Same layer as G-5 but in denser rock probably 6 m higher. The rock is plagioclase porphyry, with a dense ground mass otherwise with the same description applying to G-5.|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|3.01|Measured on crushed sample by Western Atlas Borehole Laboratories|0.550|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.005|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-7|G-7|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673797|441009|-15.39103|64.42633|162||Enn sama berg en nú 1-2 m ofan viđ G-6 og 1 m neđan viđ keilugang. Bergiđ er plagíóklas-dílótt, međ ţéttum grunnmassa annars á lýsingin viđ G-5.|Still the same rock but now 1-2 m above the G-6 and 1 m below the inclined sheet intrusions. Plagioclase porphyry with dense ground mass, otherwise similar to G-5.|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.540|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.031|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-8|G-8|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674155|441306|-15.38326|64.42880|199||Plagíóklasdílótt straumflögótt basalthraunlag međ fínkornóttum ţéttum millimassa. Sýniđ tekiđ úr blöđróttum neđri hluta lagsins. Ljósgrćnn leir fyllir blöđrur, zeólítar (m.a. skólesít og laumontít) og epidótćđar sjást.|Plagioclase porphyritic flow-banded basalt lava, with fine-grained dense matrix.  Sample taken from the vesicular bottom part of layer. Light green clay fills vesicles, epidote veins and late stage zeolites (incl. scolesite and laumontite). |Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.171|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.171|He Gas pycnometry, Western Atlas Borehole Laboratories|1.05E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.63E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-9|G-9|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674156|441310|-15.38323|64.42884|199||? sama hraunlagi og G-8 u.ţ.b. 1.5 m ofar, en ţar er bergiđ ţéttara en nokkuđ sprungiđ. |In the same lava layer as G-8 approximately 1.5 m above, where the rock is denser but somewhat fractured.|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.450|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.043|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-10|G-10|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674158|441312|-15.38319|64.42886|199||Sama hraunlag og G-9 en nú borađ ofan á topp hraunlagsins s.s. hornrétt á G-9 en samsíđa G-8. |The same lava layer as G-9 but now drilled on top of the lava layer. Sample perpendicular to G-9 but parallel to G-8.|Lava flow|Flow-top breccia|Chlorite-epidote|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.230|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.020|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-11|G-11|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675256|442208|-15.35937|64.43632|414||Úr líparíteiningu 1. Dćmigert straumflögótt ljóst og smáblöđrótt. |Rhyolite unit 1. Typical flow-banding and small vesicles.|Silicic volcanic|Rhyolite lava|Chlorite-epidote|2.66|Measured on crushed sample by Western Atlas Borehole Laboratories|0.149|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.147|He Gas pycnometry, Western Atlas Borehole Laboratories|1.05E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|3.95E-17|Measured by Western Atlas Borehole Laboratories|1.73E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-12|G-12|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675625|442316|-15.35160|64.43709|455||Móbergsbreksía úr móbergseiningu 1. Bergiđ er grágrćnt á lit, minnir einna helst á ţursaberg og er mjög epidótríkt. |Breccia from hyaloclastite  unit 1. Grey-green, reminiscent of an agglomeritic pillow breccia and is very epidote-rich. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.91|Measured on crushed sample by Western Atlas Borehole Laboratories|0.187|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.185|He Gas pycnometry, Western Atlas Borehole Laboratories|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.09E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-13|G-13|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675631|442327|-15.35145|64.43719|455||Grágrćnt túff úr móbergseiningu 1.  Bergiđ líkist mjög ţví sem kallađ er móbergsset vegna samlímdra smárra korna, ţau stćrstu all tađ 1 cm.|Grey-green tuff from tuff unit 1 og er mjög epidótríkt. The rock is very similar to what is called hyaloclastite sediment due to the cohesive small grains, the largest up to 1 cm.|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.85|Measured on crushed sample by Western Atlas Borehole Laboratories|0.342|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.342|He Gas pycnometry, Western Atlas Borehole Laboratories|4.87E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|2.76E-16|Measured by Western Atlas Borehole Laboratories|8.98E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-14|G-14|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675708|442388|-15.34979|64.43769|455||Straumflögóttur auđboranlegur líparítgangur. Gangurinn er víđast um 1-2 m á ţykkt og liggur í stefnu gilsins, ţ.e. 25°. Sýnin voru tekin samsíđa straumflögun. |Flow-banded liparite (rhyolite) dyke. Dyke is 1-2 m thick and lies parallel to the gorge, i.e. 25°. Samples were taken parallel to the flow-banding. |Silicic intrusion|Rhyolite dyke|Chlorite-epidote|2.35|Measured on crushed sample by Western Atlas Borehole Laboratories|0.237|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.234|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.40E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-15|G-15|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675165|439392|-15.36462|64.41114|87||Basalteining 1a.  Bergiđ er mjög ţétt og a.m.k. 10 m ţykkt, skoriđ af göngum úr fasa 5. Bergiđ er smásprungiđ.|Basalt unit 1a. Rock is very dense and up to 10 m thick, cut by dykes from phase 5. The rock is finely fractured.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.210|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-16|G-16|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675167|439411|-15.36456|64.41132|90||Basalteining 1a. Fínkornótt ţóleiíthraun ljósgrćnt á lit og sprungiđ milli keiluganga. Borađ ofan í áberandi epidótummyndun. |Basalt unit 1a. Fine-grained tholeiitic lava light, green in color and cut by numerous cone sheets. Drilled into a prominent epidote alteration.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|3.05|Measured on crushed sample by Western Atlas Borehole Laboratories|0.221|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.218|He Gas pycnometry, Western Atlas Borehole Laboratories|4.74E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||8.78E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-17|G-17|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675174|439414|-15.36439|64.41134|91||Basalteining 1a. Tekiđ úr sama lagi og G-16 en tekiđ úr ferskari hluta ţess. Ath. Sýnin voru nokkuđ dreifđ í laginu vegna erfiđleika viđ ađ ná A-sýni, en ţau voru nokkum veginn í sama lárétta laginu.|Basalt unit 1a. Taken from the same layer as G-16 but from a more unaltered part.  Note that the samples are somewhat scattered within the layer due to the difficulty of obtaining samples, but they were more or less in the same horizontal layer.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.93|Measured on crushed sample by Western Atlas Borehole Laboratories|0.110|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-18|G-18|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675232|439434|-15.36318|64.41149|94||Basalteining 1a. Fínkornótt blöđrótt en ţétt og dílótt ţóleiíthraunlag. Blöđrur fylltar af klóríti, epidóti o.fl.|Basalt unit 1a. Fine-grained compact porphyritic tholeiitic lava. Vesicles filled of chlorite, epidote and others. |Lava flow|Porphyritic basaltic lava|Epidote-actinolite|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-19|G-19|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675245|439433|-15.36291|64.41147|94||Basalteining 1a. Tekiđ úr sama hraunlagi og G-18, en nú borađ lóđrétt niđur í efri hluta ţess ţ.e. hornrétt á G-18. Hraunlagiđ um 3 m á ţykkt og sýniđ tekiđ úr breksíuhlutanum.|Basalt uniit 1a. Taken from same lava layer as G-18, but drilled vertically into the top part, i.e. perpendicular to G-18. Lava is about 3 m thick, and this sample was taken within the brecciated part.|Lava flow|Flow-top breccia|Epidote-actinolite|2.85|Measured on crushed sample by Western Atlas Borehole Laboratories|0.100|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.094|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-20|G-20|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675244|439445|-15.36291|64.41158|95||Basalteining 1a. Borađ í ţéttan karga milli hraunlaga, innsta kosti 2 m ţykkur grágrćnn á lit međ brúnleitri slikju.|Basalt unit 1a. Drilled in a dense crust between lava layers, at least 2 m thick, grey-green with brown weathering.|Lava flow|Flow-top breccia|Epidote-actinolite|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.540|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.051|He Gas pycnometry, Western Atlas Borehole Laboratories|4.93E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||9.87E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-21|G-21|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675235|439473|-15.36306|64.41183|99||Basalteining 1a. Borađ í stein í gilinu, sem er eins og hraunlögin fyrir ofan. Ţađ var gert vegna mikillar frostveđrunar og ţar af leiđandi myndunar á ţunnum flögum viđ yfirborđiđ. Hraunlagiđ er mjög blöđrótt grćnt á lit. |Basalt unit 1a. Drilled in a rock in the gorge, which is like the lava layers above. This was done due to severe weathering and consequently the formation of thin flakes at the surface. Lava layer is vesicular, green in color. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.85|Measured on crushed sample by Western Atlas Borehole Laboratories|0.230|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.004|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-22|G-22|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675243|439474|-15.36290|64.41184|99||Basalteining 1a. Í mynni Kráksgils. Borađ í ljósgrćnt ummyndađ basalt međ epidót, granar og aktínoólít í. Steinn var tekinn úr ţví til ađ bora í, ţar sem allt bergiđ var sprungiđ og flögótt vegna frosveđrunar. |Basalt unit 1a. At the mouth of Kráksgil. Drilled into green altered basalt with epidote, garnet, and actinolite. The rock was drilled off-site as it was very fractured and flaky due to weathering.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|3.00|Measured on crushed sample by Western Atlas Borehole Laboratories|0.160|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.153|He Gas pycnometry, Western Atlas Borehole Laboratories|1.01E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|3.55E-17|Measured by Western Atlas Borehole Laboratories|1.74E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-23|G-23|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677656|442572|-15.30919|64.43833|277||Móbergseining 2. Sýni tekiđ viđ efri mörk á grćnu túffi eđa ţar sem litaskipti eru yfir í brúnt. Ath. Vergiđ sýnir víđast hvar einkenni móbergssets, ţ.e. samlímdir smá molar í ţessu tilviki kantađir. Ekki tókst ađ ná almennilegum kjarna A og var ţví sýni merkt A+B.|Tuff unit 2. Sample taken at the upper limit of a green tuft or where the color changes to brown. It should be noted that the sample shows in most places the characteristics of a tuff sediment, ie. glued small fragments in this case angular. The normal core A could not be reached and the sample was marked A + B.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay||Measured on crushed sample by Western Atlas Borehole Laboratories||Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.000|||||||||||||||||||||||||
OS-95017_G-24|G-24|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677631|442561|-15.30971|64.43824|291||Móbergseining 2. Brúnt túff međ smábrotum og vel samlímt og er neđan viđ grćna beltiđ. Rétt ofan viđ eru dreifđir bólstrar í móberginu međ ásýnd eins og um dílótt basalthraun vćri ađ rćđa. Bólstranir hafa veriđ tengdir innbyrđis međ sprungum og er lámontít ađal ummyndunarsteind í ţeim.|Tuff unit 2. Brown tuff with small fragments and well-consolidated and is below the green belt. Directly above are distributed pillows in a hyaloclastite with appearance like porphyryitic basalt lava. Pillows are interconnected by veins with laumontite as the main depositional mineral. |Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.65|Measured on crushed sample by Western Atlas Borehole Laboratories|0.216|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.186|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-25|G-25|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677614|442552|-15.31009|64.43817|299||Móbergseining 2. Borađ í fínkornótt set međ hvarfleirs einkenni. Gćti veriđ 10-20 m ţykkt. Ţađ fćr túfflegri ásýnd ofar. Athuga ber ađ stađurinn er utan viđ Geitafellsöskjuna. |Tuff unit 2. Drilled into fine-grained sediment with glacial tillite clay character. Could be 10-20 m thick. It has a more tuffaceous appearance above. It should be noted that the site is outside the Geitafell caldera.|Hyaloclastite|Hyaloclastite sediment|Mixed-layer clay|2.64|Measured on crushed sample by Western Atlas Borehole Laboratories|0.223|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.217|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||8.88E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-26|G-26|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677596|442545|-15.31046|64.43812|308||Basalteining 2. Kargi á hraunlagi. Zeólítar eru áberandi holufyllingar (analsím, apófyllít? +) ásamt kalsíti. |Basalt unit 2. Scoraceous top of a lava layer. Zeolites are dominant secondary minerals (analcime, apophyrllite? +) along with calcite.|Lava flow|Flow-top breccia|Mixed-layer clay|2.83|Measured on crushed sample by Western Atlas Borehole Laboratories|0.191|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.188|He Gas pycnometry, Western Atlas Borehole Laboratories|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||9.87E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-27|G-27|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677573|442538|-15.31095|64.43807|318||Basalteining 2. Í sama lagi og G-26 en nú 15-20 cm neđar í ţéttari hluta lagsins, en ţađ er 1-2 m á ţykkt og er fínkorna.|Basalt unit 2. In the same layer as G-26 but 15-20 cm below in the denser part of lava; 1-2 m thick and fine-grained.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.770|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.036|He Gas pycnometry, Western Atlas Borehole Laboratories|1.48E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|2.27E-16|Measured by Western Atlas Borehole Laboratories|2.86E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-28|G-28|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677548|442528|-15.31147|64.43799|330||Basalteining 2. Borađ í breksíu milli hraunlaga, fyllta af zeólítum. Lagiđ er ţykkt međ ţunnu stáli en ţykkri breksíu. |Basalt unit 2. Drilled in a breccia between lava layers, filled with zeolites. The layer is thick with a thin compact part but a thick breccia.  |Lava flow|Flow-top breccia|Smectite-zeolite|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.169|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.166|He Gas pycnometry, Western Atlas Borehole Laboratories|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-29|G-29|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677522|442524|-15.31202|64.43797|342||Basalteining 2. Sýni tekiđ úr bergstáli í ţéttu fínkorna basalti 5m ţykku međ 1-2 m ţykkri breksíu fyrir ofan og neđan. Sýniđ sennilega tekiđ í efri hluta hraunlagsins. Strik 305° og halli 35° til austurs. |Basalt unit 2. Sample taken from rock cliff in a dense fine-grained basalt 5m thick with a 1-2 m thick breccia above and below. Sample taken from the upper part of the lava lave. Strike 305 and dip 35 to the east.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.84|Measured on crushed sample by Western Atlas Borehole Laboratories|0.120|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.004|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-30|G-30|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677494|442528|-15.31260|64.43802|353||Basalteining 2. Sýni tekiđ úr ţéttu fínkorna ţóleiítbasalthrauni. Ţađ sést nokkra metra ţykkt stál međ vel ţjöppuđum karga undir. |Basalt unit 2. Sample taken from fine-grained tholeiitic basalt lava. A outcrop several meters thick cliff with a well-compacted crust below. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-31|G-31|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677522|442515|-15.31203|64.43789|342||Móbergs- eđa basaltbreksía, sem stratigrafískt tilheyrir H-I einingu, en opnan hér í Námugili er nokkuđ ţunn, og hraunlög sem tilheyra B-II ofan viđ og B-I neđan viđ. Kjarninn er tekinn úr millimassa efni í breksíunni (ţví annars vćrum viđ í basaltsteini). Súr bergbrot sjást í breksíunni líka. Vera má ađ ţetta móberg sé flank set úr H-I. |Hyaloclastite or basalt breccia, which stratigraphically belongs to H-I unit, but the exposure here in Námagil is quite thin, and lava layers that belong to B-2 and B-1 above and below, respectively. Core is taken from groundmass of breccia (which otherwise would be in basalt). Silicic rock fragments can also be seen in the breccia. Could be that this hyaloclastite is seen in H-1.|Lava flow|Flow-top breccia|Smectite-zeolite|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.200|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.90E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-32|G-32|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Hoffellsfjall milli Skoru og Segils|677942|441135|-15.30501|64.42531|241||B-I í Hoffellsfjalli milli Skoru og Selgils.  Á ađ vera á mörkum blandlags- og klórítbeltis í ca 150 m y.s. Borađ er í ţéttan hluta hrauns sem er brúnveđrađ, fínkornótt ţóleiít, 4-5 m ţykkt. |B-I in Hoffellsfjall between Skora and Selgils. Should be at the boundary of the mixed-layer clay and chlorite alteration zones at approx. 150 m above sea level. Drilled into the dense part of the lava that is weathered-brown, fine-grained tholeiite, 4-5 m thick.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.170|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.013|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-33|G-33|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|12.8.1992|Surface|Hoffellsfjall milli Skoru og Segils|677926|441128|-15.30534|64.42526|256||Feldsat dílótt ţunnt hraun (1 m ţétt, 1 m kargi). Kjarninn er borađur hornrétt á flćđilegu í ţéttan hluta hraunsins.|Feldspar porphyritic thin lava (1 m dense, 1 m flow top breccia). Core is drilled perpendicular to the flow in the dense part of the lava.|Lava flow|Porphyritic basaltic lava|Mixed-layer clay|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.270|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.026|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-34|G-34|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Hoffellsfjall milli Skoru og Segils|677935|441127|-15.30514|64.42524|247||Úr karganum á nćsta hrauni neđan viđ, eđa úr blöđrótta hlutanum. |From the flow top breccia of the next lava below, or from the vesicular part.|Lava flow|Flow-top breccia|Mixed-layer clay|2.81|Measured on crushed sample by Western Atlas Borehole Laboratories|0.410|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.037|He Gas pycnometry, Western Atlas Borehole Laboratories|6.91E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|9.87E-19|Measured by Western Atlas Borehole Laboratories|7.90E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-35|G-35|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Stóraskriđugil|677505|439292|-15.31629|64.40904|222||Stóraskriđugil, í klórítbelti fremur en blandlagsbelti.  Ţétt fínkornótt ţóleiít hraun, 5-6 m ţykkt, međ 1 m kargalagi ofaná. Kjarnarnir eru borađir inn í hrauniđ samsíđa flćđiböndum, 1 m ofan viđ botns hraunsins. |Stóraskriđu gil, in chlorite zone rather than mixed layer clay zone. Dense fine-grained tholeiitic lava, 5-6 m thick, with 1 m thick flow top breccia  on top. Core is drilled into the lava parallel to the flow banding, 1 m above the bottom of the lava.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.120|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-36|G-36|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Stóraskriđugil|677497|439297|-15.31645|64.40909|229||Borađ í blöđróttan efri hluta sama hrauns og G-35. Blöđrótti hlutinn er ca. 1.5-2 m á ţykkt og er kjarninn tekinn 30-40 cm ofan ţétta hlutans. |Drilled into the vesicular upper part of the same lava as the G-35. The more vesicular part is ca. 1-5 m thick and the core is taken 30-40 cm above the dense part. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|3.09|Measured on crushed sample by Western Atlas Borehole Laboratories|0.137|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.054|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-37|G-37|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Stóraskriđugil|677507|439302|-15.31622|64.40912|221||Sama hraun og G-36/36 en ca 1 m ofan ţétta hlutans. Ţétta sýni er áberandi blöđróttara en G-36.|The same lava as G-36 but about 1 m above the dense part. This sample is clearly more vesicular than G-36. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.93|Measured on crushed sample by Western Atlas Borehole Laboratories|0.169|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.169|He Gas pycnometry, Western Atlas Borehole Laboratories|7.90E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.78E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-38|G-38|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Stóraskriđugil|677514|439300|-15.31609|64.40910|216||Ţétt ţóleiít hraun ca 4 m ţykkt međ 1 m karga. Sýniđ er tekiđ ca 1 m frá botni til samanburđar viđ G-35 í sama klóríđbelti. Blöđrur sjást vel međ berum augum og prímer groppa ţví líklega hćrri. Epidót sést ekki í sýninu en ađeins vottar fyrir ţví í lausu kargaefni í farvegi ţessa gils. |Dense tholeiitic lava about 4 m thick with 1 m thick flow-top breccia. Sample is taken ca. 1 m from the bottom for comparison with G-35 in the same chlorite belt. Vesicles are obvious to the eye and primary porosity likely higher. Epidote not visible in sample but there are traces within the loose flow-top breccia in the driveway into the valley.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.140|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.006|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-39|G-39|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Stóraskriđugil|677560|438699|-15.31586|64.40369|70||Súrt rhyolít hraun úr botni B-I myndunnar. Fullt af epidóti. Sýniđ var tekiđ í handsýni til borunnar í Reykjavík vegna hörku. |Rhyolite lava from the base of the B-I formation. Abundant epidote. Sample was taken as hand-sample to core in Reykjavik due to hardness. |Silicic volcanic|Rhyolite lava|Epidote-actinolite|2.67|Measured on crushed sample by Western Atlas Borehole Laboratories|0.720|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.070|He Gas pycnometry, Western Atlas Borehole Laboratories|6.91E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|9.87E-18|Measured by Western Atlas Borehole Laboratories|1.58E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-40|G-40|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Geitafellsgil í mynni gilsins|673839|440346|-15.39094|64.42037|84||Geitafellsgabbró. Sýni tekiđ úr Geitafellsgabbóri, sem er innskota fasi 2 í eldstöđinni. Borađ var í laust grjót úr grjótnámu (Seđlabankinn). |Geitafell gabbro. Sample taken from Geitafell gabbro, which is a phase 2 intrusion within the volcano. Drilled into loose stones from the rock quarry (central bank). |Basaltic intrusion|Gabbro|Epidote-actinolite|3.05|Measured on crushed sample by Western Atlas Borehole Laboratories|0.800|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-41|G-41|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Geitafellsgil í mynni gilsins|673813|440420|-15.39140|64.42105|85||Gangur úr fasa 5 í gabbrói. Berg er međalgróft og blöđrur sjást. |Dyke from phase 5 in gabbro. Rock is medium-coarse grained and vesicles are visible.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.400|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.034|He Gas pycnometry, Western Atlas Borehole Laboratories|2.94E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.14E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-42|G-42|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|13.8.1992|Surface|Geitafellsgil í mynni gilsins|673825|440424|-15.39115|64.42108|87||Gangur úr fasa 10 (?) í gabbrói einnig međ ađliggjandi granófýr. Gangurinn er blöđróttur. |Dyke from phase 10 (?) In gabbro also adjacent to granophyre. The dyke is vesicular.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.009|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-43|G-43|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673823|440421|-15.39119|64.42105|87||Sýni tekiđ úr 60 cm ţykkum gangi, sem var dílóttur inn viđ miđju. Sýni var tekiđ utan viđ dílótta hlutann (innskotafasi 6).|Sample taken from 60 cm thick dyke, that becomes more porphyritic towards the middle. Sample was taken out of the porphyritic part (intrusive phase 6).|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.290|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.021|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-44|G-44|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673815|440422|-15.39135|64.42106|86||Sýni tekiđ úr sama gang og G-43 en nú úr dílóttari hlutanum. (innskotafasi 6).|Sample taken from same dyke as G-43 but now from the more porphyritic part (intrusive phase 6)|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.190|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.014|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-45|G-45|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673827|440811|-15.39065|64.42454|129||Sýni úr keilugangi, sem tilheyrir fasa 6. Gangurinn er 80 cm ţykkur og blöđróttur viđ kćliflötinn og dílóttur.|Sample from a cone sheet belonging to phase 6. The cone sheet is 80 cm thick and more vesicular with cooling textures and is porphyritic.|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.93|Measured on crushed sample by Western Atlas Borehole Laboratories|0.140|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-46|G-46|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673824|440818|-15.39070|64.42460|129||Úr sama keilugangi og G-45 en nú ţvert á ganginn í gegnum blöđróttan jađar.|From the same cone dyke as G-45 but now across the dyke through a more vesicular part. |Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.120|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-47|G-47|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673828|440836|-15.39060|64.42477|134||Úr keilugangi, sem tilheyrir fasa 6. Gangurinn er 80 cm ţykkur. Beriđ er dílótt og útfellingar í sprungum. Gangaţéttleiki er 95-100%. |From cone sheet that belongs to phase 6. Sheet is 80 cm thick.Rock is porphyritic with vein fillings. Intrusive intensity is 95-100 %.|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.90|Measured on crushed sample by Western Atlas Borehole Laboratories|0.270|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories|1.04E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.18E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-48|G-48|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673826|440846|-15.39062|64.42486|135||Sýni tekiđ úr dólerítgangi, sem tilheyrir fasa 7. Gangurinn er dílóttur inn ađ miđju, en hann er um 1.5 m á ţykkt. Sýni tekiđ úr hliđ hans ţar sem fylla hefur brotnađ úr. Stefna 270° og halli 60°.|Sample taken from doleritic dyke that belongs to phase 7. Dyke is porphyritic in central part and is 1.5 m thick. Sample taken from the side where where section has fallen down. Strike 270° and dip 60°.|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.97|Measured on crushed sample by Western Atlas Borehole Laboratories|0.200|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.018|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-49|G-49|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673825|440850|-15.39064|64.42489|136||Sýni tekiđ úr keilugangi úr fasa 5. Gangurinn er yfir 1 m á ţykkt. |Sample taken from cone sheet from phase 5. Sheet is over 1 m thick.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.320|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.011|He Gas pycnometry, Western Atlas Borehole Laboratories|2.81E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.99E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-50|G-50|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673825|440857|-15.39064|64.42495|137||Sýni tekiđ úr dulkornóttum gangi sem hríslast ofan  viđ G-49 og er 5-15 cm ţykkur. |Samples taken from a micro-crystalline dyke that winds above G-49 and is 5-15 cm thick.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.90|Measured on crushed sample by Western Atlas Borehole Laboratories|0.150|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-51|G-51|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673826|440865|-15.39061|64.42503|139||Sýni tekiđ úr keilugangi, sem tilheyrir fasa 5. Steinn var tekinn úr ganginum og borađur.|Sample taken from cone sheet from phase 5. Rock was taken from the dyke and drilled.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.068|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.48E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-52|G-52|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673832|440867|-15.39048|64.42504|141||Sýni tekiđ úr 1.5 m ţykkum gangi úr fasa 5,  rétt viđ G-51. |Sample taken from 1.5 m thick dyke from phase 5, right next to G-51.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.93|Measured on crushed sample by Western Atlas Borehole Laboratories|0.250|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.021|He Gas pycnometry, Western Atlas Borehole Laboratories|9.48E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.05E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-53|G-53|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673830|440873|-15.39050|64.42509|142||Tilheyrir fasa 4 og er hann súr. Gangurinn er líklega 50-60 cm ţykkur og er annar jađarinn ađ minnsta kosti mikiđ brotinn. |Rhyolitic dyke from phase 4, 50-60 cm thick, one of the boundaries is heavily fractured.|Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.640|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.062|He Gas pycnometry, Western Atlas Borehole Laboratories|4.93E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||6.91E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-54|G-54|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673830|440878|-15.39050|64.42514|143||Sýni úr dólerítgangi, sem tilheyrir fasa 12. Gangurinn er 1-2 m á ţykkt. |Doleritic dyke belonging to phase 12. Dyke is 1-2 m thick.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.520|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.004|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-55|G-55|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670968|443422|-15.44684|64.44937|165||Úr porfýrískum gangi, sem tilheyrir fasa 10. Gangurinn er 4 m á ţykkt og sker móberg en rétt viđ er súr gangur úr fasa 11. Stefna 38°.|Porphyritic dyke from phase 10, 4 m thick, cuts tuff but right next to it is a rhyolitic dyke from phase 11. Strike 38°.|Basaltic intrusion|Porphyritic basaltic intrusion|Chlorite-epidote|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.150|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.90E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-56|G-56|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670965|443417|-15.44690|64.44933|165||Sýni tekiđ úr sama gangi og G-55 en nú viđ jađar hans. Ath. Gangurinn er mikiđ brotinn og liggja ćđar langs og ţvers.|Sample taken from same dyke as G-55 but now at the edge of it. Dyke is very fractured and cross-cut by veins horizontally and vertically. |Basaltic intrusion|Porphyritic basaltic intrusion|Chlorite-epidote|2.81|Measured on crushed sample by Western Atlas Borehole Laboratories|0.230|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.014|He Gas pycnometry, Western Atlas Borehole Laboratories|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||9.87E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_G-57|G-57|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670952|443399|-15.44719|64.44918|167||"Líklega ""feeder dyke"" og ţá fasi 1. Smá stubbur sést af honum í móbergsmyndun 2 og er 1 m á ţykkt. Epidót sést á kćliflötum og súlfíđ sést í fínkornóttu gangberginu. Stefna 163°."|Likely feeder dyke from phase 1. A small piece of it is visible in tuff formation 2 and is 1 m thick. Epidote is visible on cooling dyke boundary and sulfide visible in fine-grained gangue. Strike 163°.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.81|Measured on crushed sample by Western Atlas Borehole Laboratories|0.360|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.025|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-58|G-58|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670949|443368|-15.44730|64.44891|168||Móbergseining 2. Sýni tekiđ skammt frá G-57 og rétt viđ fasa 11, sem er súr. Bergiđ er mjög túfflegt. Ţetta er rétt viđ jökuljađarinn. |Hyaloclastite unit 2. Sample taken close to G-57 and close to phase 11 which is acidic. Rock looks tuffeceous. This is right by the edge of the glacier.|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.910|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.089|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-59|G-59|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670945|443346|-15.44740|64.44871|168||Keilugangur sem tilheyrir fasa 8 og sker móbergsmyndun 2. Gangurinn er 50-80 cm ţykkur og var sýniđ borađ úr hliđ hans. Hann er fínkornóttur, blöđróttur, stakdílóttur og sést epidót í ţeim.|Cone sheet from phase 8 that cuts hyaloclastite formation 2. Dyke is 50-80 cm thick and sample was drilled from the side of it. It is fine-grained, vesicular, sparsely porphyritic with epidote visible.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.92|Measured on crushed sample by Western Atlas Borehole Laboratories|0.400|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-60|G-60|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670939|443339|-15.44753|64.44865|169||Dólerítkeilugangur, sem tilheyrir fasa 5. Sýni var borađ ţvert á hann ađ ofanverđu. Mikiđ krađak var af flestum Innskotafösunum ţarna í nagrenninu. |Doleritic cone sheet belonging to phase 5. Sample was drilled directly into it from above. A lot of evidence from other intrusive phases are present in the area.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.82|Measured on crushed sample by Western Atlas Borehole Laboratories|0.200|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-61|G-61|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670934|443330|-15.44765|64.44857|169||Sýni úr keilugangafasa 6. Hann er pofrýrískur og u.ţ.b. 1 m á ţykkt. Sýniđ var tekiđ ţvert á stuđlun.|Sample from cone sheet phase 6, porphyritic and approximately 1 m thick. Sample was taken at right angle to the column.|Basaltic intrusion|Porphyritic basaltic intrusion|Chlorite-epidote|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.360|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.010|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-62|G-62|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670937|443320|-15.44759|64.44848|169||Gangberg, sem tilheyrir fasa 7. Hann er porfýrískur og grófkornóttur, grćnleitur ađ sjá og epidótríkur. Epidót virđist korna í stađ plagíóklas í dílum. Sýni var tekiđ í gegnum jađar gangsins samsíđa stuđlun.|Dyke from phase 7, porphyritic and coarse-grained, green and epidote rich. Epidote is seen to replace plagioclase. Sample taken perpendicular to the dyke boundary and along the entablature.|Basaltic intrusion|Porphyritic basaltic intrusion|Chlorite-epidote|2.83|Measured on crushed sample by Western Atlas Borehole Laboratories|0.370|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.010|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-63|G-63|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670918|443299|-15.44801|64.44830|171||Handsýni var tekiđ úr súrum gangi til ţess ađ bora í bćnum. Sýniđ nokkurn veginn úr miđjum ganginum, en hann er nokkra metra ţykkur (Innskotafasi 11).|Hand-sample taken from acidic dyke to drill back in Reykjavik. Sample taken near middle of the dyke, but it is a few meters thick. Intrusive phase 11.|Silicic intrusion|Rhyolite dyke|Chlorite-epidote|2.63|Measured on crushed sample by Western Atlas Borehole Laboratories|0.260|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.017|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-64|G-64|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670920|443275|-15.44800|64.44808|172||Dólerítgangur, sem tilheyrir fasa 12. Sýniđ er tekiđ nokkurn veginn í miđjum ganginum, sem er um 4 m ţykkur. Utan í ganginum eru 10-40 cm ţykkar ćđar af kalsíti, kvarsi og súlfíđum.|Doleritic dyke from phase 12. Sample is taken near the middle of the dyke, which is 4 m thick. Outside of the dyke margin are 10-40 cm thick veins of calcite, quartz, and sulfides.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.92|Measured on crushed sample by Western Atlas Borehole Laboratories|0.490|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-65|G-65|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670920|443272|-15.44801|64.44806|172||Sýni tekiđ tekiđ í 0.5-1 m breiđri sónu á jađri dólerítsgangsins, sem sýni G-64 var tekiđ úr. |Sample taken from 0.5-1 m broad zone adjacent to the doleritic dyke where sample G-64 was taken from.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.81|Measured on crushed sample by Western Atlas Borehole Laboratories|0.400|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-66|G-66|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670912|443258|-15.44819|64.44794|172||Basaltbreksía líklega tengd hraunlögum, en erfitt er ađ meta ţykkt ţeirra. Sennilega fáeinir metrar á ţykkt. |Basalt breccia probably associated with lava flow, but their thickness is difficult to estimate. Probably a few meters thick.|Lava flow|Flow-top breccia|Chlorite-epidote|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.200|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-67|G-67|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670901|443258|-15.44843|64.44794|173||Sýni tekiđ um 5m ofan viđ G-66 í fínkornóttu basalt hraunlagi, en ţađ er fínblöđrótt og ţćr fylltar af klóríti. |Sample taken about 5 m above G-66 in a fine-grained basaltic lava layer, which has small vesicles filled with chlorite.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.85|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-68|G-68|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Innst viđ Ţverá austan Efstafellsness|672082|442610|-15.42470|64.44154|223||Sýni tekiđ úr bergstáli fínkorna ţóleiítshraunlags, en skammt frá sýnatökustađnum er 20-40 cm ţykk kalsítćđ. |Sample taken from rock-cliff, a fine-grained, tholeiitic lava, and a a short distance from the sampling site is a 20-40 cm thick calcite vein.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.84|Measured on crushed sample by Western Atlas Borehole Laboratories|0.150|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.005|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_G-69|G-69|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|15.8.1992|Surface|Norđan Kráksgils|675118|439360|-15.36564|64.41088|79||Hraun úr basalteiningu B-I rétt norđan Kráksgils í aktínólít belti.  Hrauniđ er ţétt ásýndar, ţóleiít, 4-6 m ţykkt, fínkornótt. Borađ var í mitt hrauniđ samsíđa flćđi (halli 10-15°).|Lava from basalt unit B-I just north of Kráksgil within an actinolite zone. The lava looks dense, tholeiitic, 4-6 m thick and fine-grained. Drilled into the middle of the lava parallel to the flow direction (dip 10-15°).|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.88|Measured on crushed sample by Western Atlas Borehole Laboratories|0.500|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-1|H-1|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361550|442011|-21.87706|64.45156|172||Hraunlag undir eđa á milli dólerít keiluganga. Bergiđ er fínkorna,  blöđrótt, ljósgrćnt í brotsári. Blöđrur helmings fylltar til tómar, svo og einnig fylltar, mest af klóríti. |Lava layer under or between doleritic cone sheets. Rock is fine-grained, vesicular, light-green in the fracture planes. Vesicles half-filled to empty, with some filled, mostly of chlorite.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.88|Measured on crushed sample by Western Atlas Borehole Laboratories|0.138|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.134|He Gas pycnometry, Western Atlas Borehole Laboratories|1.58E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.86E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-2|H-2|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361550|442011|-21.87706|64.45156|172||Keilugangur (hćđ 105 m y. s.), um 5 m ofan viđ hraunlagiđ. Bergiđ er fín-međalkorna plagíóklas-dílótt (smáir dílar). |Cone sheet (elevation 105 m asl) about 5 m above lava flow. Rock is fine-medium grained and plagioclase porphyritic (small phenocrysts).|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.90|Measured on crushed sample by Western Atlas Borehole Laboratories|0.350|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.026|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-3|H-3|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361562|442031|-21.87683|64.45175|180||Grannberg viđ 1 m ţykkan keilugang (H-2) ađ ofanverđu. Bergiđ er fínkorna, ljósgrágrćnt, blöđrótt og blöđrufyllt af a: svörtum leir > klórít, b: Hvítar fyllingar međ epidóti og etv granati. Bergiđ er plagíóklasdílott. |Neighboring rock to a 1 m thick cone dyke (H-2) at the top. Rock is fine-grained, light-grey-green, vesicular, and vesicle-filled with a: dark clay > chlorite, b: White precipitate with epidote and perhaps garnet. Rock is plagioclase porphyritic. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.90|Measured on crushed sample by Western Atlas Borehole Laboratories|0.144|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.142|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.18E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-4|H-4|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361591|442056|-21.87625|64.45198|193||Gabbró eđa grófkorna dólerít keilugangur, flögótt berg (hćđ 115 m).  Fyrsta haftiđ í gilinu. Bergiđ grá-grćnleitt. |Gabbro or coarse-grained doleritic cone sheet, flaky rock (elevation 115 m). The first barrier in the gorge. The rock is gray-greenish.|Basaltic intrusion|Gabbro|Epidote-actinolite|2.92|Measured on crushed sample by Western Atlas Borehole Laboratories|0.290|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.027|He Gas pycnometry, Western Atlas Borehole Laboratories|1.97E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.47E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-5|H-5|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361603|442071|-21.87601|64.45213|201||Kolummyndađ hraunlag milli keiluganga. Grćnleitt ađ lit, fínkorna, blöđrótt. Epidót, granat? Og magnetít. Bergiđ mjög flögótt.|Intensely altered  basalt between cone sheets. Light green color, fine-grained, vesicular. Epidote, garnet? And magnetite. Rock very flaky. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.167|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.158|He Gas pycnometry, Western Atlas Borehole Laboratories|1.96E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.24E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-6|H-6|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361624|442095|-21.87559|64.45234|213||Keilugangur (150m hćđ). Hlíđarnar mjög skriđuorpnar og lítiđ ađ sjá annađ en keiluganga međ reglulegu millibili. Keilugangurinner um 1 m breidd, grófkorna og grár ađ lit. Feltmynd sem sýnir afstöđu sýna H-6, 7 og 8.|Cone sheet (150 m elevation). Scree covered slope and little to see other than evenly distributed cone sheets. Sheet is about 1 m thick, coarse-grained and grey-colored. Field picture shows sampling points for H-6, 7 and 8.|Lava flow|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.91|Measured on crushed sample by Western Atlas Borehole Laboratories|0.190|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.013|He Gas pycnometry, Western Atlas Borehole Laboratories|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.09E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-7|H-7|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361620|442086|-21.87567|64.45227|209||Mjög blöđrótt hraunlag rétt viđ kontaktinn á keiluganginum (sem sýni H-8 er tekiđ úr). Bergiđ er grćnt ađ lit. Hvítar blöđrufyllingar en gulur blćr bendir til viđveru epidóts. Bergiđ fínkorna grátt. Gćti veriđ viđ lagmót. Plagíóklas dílar sjást. |Very vesicular lava right at the contact of the cone dyke (from which H-8 is taken from). Rock is green colored. White vesicle fillings but yellow tint suggests the presence of epidote. Rock is fine-grained and grey. Could be at layer boundary. Plagioclase phenocrysts are visible. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.70|Measured on crushed sample by Western Atlas Borehole Laboratories|0.180|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.101|He Gas pycnometry, Western Atlas Borehole Laboratories|2.46E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.32E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-8|H-8|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361620|442086|-21.87567|64.45227|209||Keilugangur, borađ ofan í miđju hans. Gráleitt međal-grófkorna og líklega plagíóklasdílótt. Ca. 1 m ţykkt.|Cone sheet, drilled above into the middle of it. Grey-colored medium-coarse grained and likely plagioclase porphyryitic. Ca. 1 m thick. |Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.92|Measured on crushed sample by Western Atlas Borehole Laboratories|0.310|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.026|He Gas pycnometry, Western Atlas Borehole Laboratories|8.88E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-9|H-9|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361628|442091|-21.87552|64.45231|212||Hraunlag milli keiluganga. Fínkorna og ţétt og smásprungiđ grátt ađ lit. Sýniđ tekiđ rétt ofan viđ H-8. Epidót sést í sprungum.|Lava flow between cone sheet. Fine-grained and dense with small veins grey in color. Sample taken right above H-8. Epidote visible in fractures.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.90|Measured on crushed sample by Western Atlas Borehole Laboratories|0.430|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.029|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-10|H-10|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361735|442248|-21.87346|64.45377|282||Borađ ofan í fínkorna ţétt basalt í hornfels-sónu. Um 1 m neđan viđ keilugang. Smásprungiđ og smáblöđrótt og grásvart ađ lit. Ekki unnt ađ geta sér til um ţykkt vegna kelugangnakrađaks. |Sample taken above fine-grained, dense basalt in hornfels zone. Around 1 m next to cone dyke. Finely-fractured with small vesicles and grey-black in color. Not possible to estimate thickness due to cone-sheet interference|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.750|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.070|He Gas pycnometry, Western Atlas Borehole Laboratories|1.34E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.17E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-11|H-11|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361744|442259|-21.87326|64.45387|286||Hraunlag úr hornfelsummyndun í komplex af göngum og keilugöngum (hćđ 175 m). |Lava flow from hornfels zone in a complex of dykes and cone dykes (elevation 175 m)|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.110|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-12|H-12|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361752|442269|-21.87312|64.45396|289||Gangur strik 30-35° međ 60-70° austlćgum halla og 1-1.5 m ađ ţykkt. Ţétt sprungulaust og kristöllun breytileg í berginu.|Dyke striking 30-35° with 60-70° easterly dip, 1-1.5 m thick.  Dense, without fractures, and variable crystallization in the rock.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|||||0.000|||||||||||||||||||||||||
OS-95017_H-13|H-13|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361780|442289|-21.87254|64.45414|296||Fínkornótt blöđrótt hornfels basalt í gangakomplex eins og H-12, en ţetta er austan viđ  N-S gangana, sem lćkurinn liđast eftir. Bergiđ er mjög ummyndađ í kringum blöđrunar, er dökkgrćnt í blöđrum en lýsist út frá ţeim. |Fine-grained vesicular hornfels basalt in dyke complex like H-12, to the east of N-S dykes parallel to the stream. Rock is very altered around the vesicles, dark-green but gets brighter away from them.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|3.01|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.004|He Gas pycnometry, Western Atlas Borehole Laboratories|1.22E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|2.74E-16|Measured by Western Atlas Borehole Laboratories|1.36E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-14|H-14|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361802|442277|-21.87207|64.45405|292||Gabbró áđur en ţađ verđur grófast, mćtti kalla međalkorna (hćđ 250 m). Ţétt sprungulaust gabbró, grćnleitt í annan endann, etv. vegna yfirborđsveđrunar.|Medium-grained gabbro (250 m elevation). Dense, vesicle-free gabbro, green colored at one end, perhaps to due surface weathering. |Basaltic intrusion|Gabbro|Epidote-actinolite|3.08|Measured on crushed sample by Western Atlas Borehole Laboratories|0.250|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.022|He Gas pycnometry, Western Atlas Borehole Laboratories|7.90E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.68E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-15|H-15|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361811|442280|-21.87190|64.45408|293||Gabbró um 10 m ofar en H-14. Ţétt blöđrulaust gabbró.|Gabbro about 10 m above H-14. Dense, compact gabbro with no vesicles. |Basaltic intrusion|Gabbro|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.180|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.016|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||8.88E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-16|H-16|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361816|442286|-21.87179|64.45413|295||Fínkorna gabbró í 230 m hćđ einhvers konar utaná liggjandi. |Fine-grained gabbro at 230 m elevation, probably near the outer bounday.|Basaltic intrusion|Gabbro|Epidote-actinolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.005|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-17|H-17|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361863|441239|-21.86984|64.44478|92||Fínkorna ţóleiít hraunlag, Mjög flögótt, svipađ og H-18 hvađ varđar ţykkt og útlit. |Fine-grained tholeiitic lava.  Very flaky, similar to H-18 in terms of thickness and appearance.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.300|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.006|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-18|H-18|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361874|441266|-21.86963|64.44502|94||Fínkorna grásvart ţóleiít hraunlag, Ţétt en blöđrótt til jađranna. Lágmarksţykkt 5 m. |Fine-grained gray-black tholeiitic lava flow, Dense but vesicular on the edges. Minimum thickness 5 m.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.300|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.007|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-19|H-19|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361876|441269|-21.86959|64.44505|94||Blöđrótt ţóleiít hraunlag, ca. 2 m frá toppi, en ţar eru laggangar. Bergiđ er grágrćnt og verulega ummyndađra en í sýninu á undan. Klórít, epidót, lámontít o.fl. Ţykkt >5 m.|Vesicular tholeiite lava layer, approx. 2 m from the top, near to layered sills. The rock is gray-green and actually more altered than the sample below. Chlorite, epidote, laumontite, and others. Thickness >5 m.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.450|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.034|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-20|H-20|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361883|441278|-21.86945|64.44513|94||Samskonar sýni og H-19. Mjög smáblöđrótt, fylltar og um 4 óreglulegar sprungur. |Same kind of sample as H-19. Very finely-vesicular, filled, and around 4 irregular veins.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.87|Measured on crushed sample by Western Atlas Borehole Laboratories|0.540|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||6.91E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-21|H-21|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361959|441316|-21.86792|64.44550|97||Hraunlag, borađ um 1.5 m frá toppi lags sem er a.m.k.. 2.5 m ţykkt en ekki sést í botninn. Um 1.5 m fyrir ofan er um hálfs metra ţykkur laggangur. Bergiđ er blöđrótt. |Lava layer, drilled about 1.5 m from the top of the layer which is at least 2.5 m thick but not visible at the bottom. About 1.5 m above is a half-meter thick sill. Rock is vesicular.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.500|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.046|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-22|H-22|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361959|441321|-21.86793|64.44555|97||Kargi ofan á laggangi. Ath. veđrun kargans ávöl líkt og sést í ólivín ţóleiít en aftur á móti er veđrun hraunanna mjög ţóleiítleg.  Karginn er nánast svartur, en víđa verđur hann snögglega ljósgrćnn vegna ummyndunar. |Flow-top breccia on top of a basaltic sill. The spherical weathering in the breccia, similar as observed in olivine tholeiite, but on the other hand tholeiitic weathering is suggested. The breccia is almost black (hornfelsic?), but in many places it appears light green and chloritic.|Lava flow|Flow-top breccia|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.300|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.029|He Gas pycnometry, Western Atlas Borehole Laboratories|1.66E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|2.47E-16|Measured by Western Atlas Borehole Laboratories|1.77E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-23|H-23|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361974|441352|-21.86765|64.44583|99||Í um 2 m ţóleiítkarga ofan á 3-5 m ţykku hraunlagi. |Within a 2m tholeiitic flow top breccia on top of a 3-5 m thick lava layer|Lava flow|Flow-top breccia|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.171|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.170|He Gas pycnometry, Western Atlas Borehole Laboratories|3.65E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.30E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-24|H-24|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361976|441360|-21.86761|64.44590|100||Í 3-5 m ţykku ţóleiít hraunlagi ofan á hraunlagi sem H-23 var tekiđ úr. |Within a 3-5 m thick tholeiitic lava flow on top of the lava from which sample H-23 was taken.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.310|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories|2.76E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.26E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-25|H-25|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361984|441371|-21.86745|64.44600|101||Mjög svipađar ađstćđur og í H-23 en ekki eins skýrar vegna skriđu. |Very similar to H-23 but not as clear due to scree cover.|Lava flow|Flow-top breccia|Chlorite-epidote|2.88|Measured on crushed sample by Western Atlas Borehole Laboratories|0.880|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.084|He Gas pycnometry, Western Atlas Borehole Laboratories|3.26E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-26|H-26|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar viđ Leirá|361986|441377|-21.86742|64.44606|102||Smáblöđrótt ađ mestu leirfylltar og sprungulaust. |Small vesicles, mostly clay-filled and rock apparently unfractured. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.260|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories|1.88E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.17E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-27|H-27|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Votuklettagil upp ađ Hrossatungugabbrói|361439|448364|-21.88538|64.50844|197||Súrt setlag rétt ofan viđ gömlu vatnsveitu Borgarness. Mjög flögótt, og í ţví má sjá kúluummyndun, ţ.e. dökkgráleitar kúlu eđa rákir sem rađa sér línulega og hafa meiri ummyndun en ljósara bergiđ í kring. Ljósgrćnt sýni tekiđ úr steini í skriđunni. Glerstrúktúr sést í berginu, og eru porur fylltur, 4 sprungur undir 45° horni. |Highly altered basaltic sediment just above the old Borganes water supply. Very flow-banded, with spherical weathering, i.e. dark-grey spheres or streaks that are linearly oriented and have more alteration (hornfelsic?) than the surrounding lighter colored rock. A light-green sample was taken from a stone in the scree. Glass structure can be seen in the rock, which has filled pores and 4 veins under 45° angle. |Sediment|Sediment|Chlorite-epidote|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.195|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.190|He Gas pycnometry, Western Atlas Borehole Laboratories|2.47E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||6.42E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-28|H-28|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361426|448314|-21.88561|64.50800|200||Blöđrótt fínkorna basalt nálćgt toppi. Opnur í lagiđ takmarkađar (130 m hćđ). Töluvert sést af zeólítum í blöđrum, smáum og stórum. Epidót. |Near top of a fine grained basalt lava. Limited exposure at the top of layer (130 m elevation). Numerous zeolites in vesicles, small and large. Epidote.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.140|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.093|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-29|H-29|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361428|448316|-21.88557|64.50801|199||Tekiđ úr hraunlagi í lćkjarfarvegi skammt ofan viđ H-28 (130 m). Borađ rétt viđ innskot og hluti sýnis gćti veriđ úr kontakti.|Lava flow in a stream channel close to H-28 (130m elevation). Drilled right next to an intrusion and a part of the sample could be from the contact. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.580|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.035|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-31|H-31|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361390|448140|-21.88619|64.50642|212||Fínkorna gangur. straumflögóttur og eru hvítar útfellingar í flöguninni (hćđ 140 m). Stefna 20°. Allt ađ 4 m og er samsettur. |Fine-grained dyke, flow-banded with white deposition in the layers (140 m elevation). Strike 20°. Up to 4 m thick and is compact. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.200|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-32|H-32|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448097|-21.88611|64.50603|214||Gangur svipađur og H-31. Tekiđ úr miđju hans. Stakblöđrótt og fyllt, nokkrar microsprungur undir 20-30° horni. |Dyke similar to H-31. Sample from the middle of it. Large, filled vesicles, some microfractures with less than 20-30° angle.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|||||0.000|||||||||||||||||||||||||
OS-95017_H-33|H-33|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448074|-21.88609|64.50583|218||Mjög klórítfyllt hraun, blöđrótt og međ epidóti. Sýniđ sennilega tekiđ í efri hluta hraunlagsins. Sýnastađurinn er rétt ofan viđ gilmótin.|Very chlorite rich lava, vesicular and with epidote. Sample probably taken from the upper part of the lava layer. Sample point is directly above the gorge. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.75|Measured on crushed sample by Western Atlas Borehole Laboratories|0.800|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-34|H-34|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361394|448046|-21.88601|64.50558|221||Blöđrótt berg líkt og hraunlag um 1 m  NV viđ ganginn í H-31 ca. Nokkuđ blöđrótt og fyllt. Engar sprungur.|Vesicular rock similar to a lava flow about 1 m northwest of the dyke that H-31 was sampled from. Somewhat vesicular and filled. No veins. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.85|Measured on crushed sample by Western Atlas Borehole Laboratories|0.110|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-35|H-35|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361393|448044|-21.88604|64.50556|222||Inni í miđjum ganginum. Ţétt-smáblöđrótt og fyllt, engar sprungur.|Sample taken in the middle of a dyke. Dense, with small, filled vesicles, no veins. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.88|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-36|H-36|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361393|448035|-21.88602|64.50548|223||Gangur. Í H-36 er gangurinn smáblöđróttur og í kjarnanum eru ţćr fylltar klóríti. Mjög smáblöđrótt og ţćr fylltar, engar sprungur.|Dyke. The dyke has micro-vesicles and in the center  they are filled with chlorite. Very small, filled vesicles, no veins. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.84|Measured on crushed sample by Western Atlas Borehole Laboratories|0.100|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-37|H-37|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448021|-21.88604|64.50536|226||Borađ í hraun í ca. 1 m fjarlćgđ frá gangi. Bergiđ er fínkorna og ţétt og engar blöđrur (etv ekki hraun).|Lava ca. 1 m away from dyke. Rock is fine-grained and compact with no vesicles (maybe not a lava).|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.340|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.005|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-38|H-38|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361390|448008|-21.88607|64.50523|229||Keilugangur strik 120°, um 1 m ađ ţykkt. Ţétt, blöđrur sjaldgćfar og ţá fylltar, sprungulaust.|Cone sheet striking 120 degrees, around 1 m thick. Compact, few filled vesicles, no veins.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.91|Measured on crushed sample by Western Atlas Borehole Laboratories|0.750|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.073|He Gas pycnometry, Western Atlas Borehole Laboratories|2.04E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.65E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-39|H-39|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361314|447831|-21.88747|64.50362|266||Sýni tekiđ úr miđjum laggangi sem liggur á milli tveggja hraunlaga. Gangurinn um 40-50 cm ţykkur. Ţétt án sprunguna. |Sample taken from the middle of a sill lying between two lava flows. Intrusion is 40-50 cm thick. Compact without veins.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.260|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-40|H-40|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361310|447830|-21.88755|64.50361|267||Efra yfir borđ á hrauni rétt fyrir ofan H-39. Virđist stakblöđrótt og fyllt, ca. 8 óreglulegar sprungur.|Upper surface of lava just above H-39. Appears to have sparse, filled vesicles, ca. 8 irregular veins. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.290|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.022|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-41|H-41|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361305|447818|-21.88765|64.50350|271||Breksía ofan á hraunlagi, grćnleitt ađ lit smásprungiđ.  Bergiđ er dökkt ađ sjá en viđ blöđrur og sprungur lýsist ţađ mjög vegna aukinnar ummyndunar. Ath. ekki unnt ađ sjá ţykkt hraunlagsins ţar sem ţađ sést ađeins ofan á ţađ í klöppinni. Erfitt ađ ná í A-sýni. |Breccia on top of a lava flow, greenish in color, micro fractured. The rock is dark coloured,vesicle and veins are lighter coloured due to increased alteration. Note that it is not possible to see the thickness of the lava layer as only the top of it is visible. Difficult to obtain the A-sample. |Lava flow|Flow-top breccia|Chlorite-epidote|2.84|Measured on crushed sample by Western Atlas Borehole Laboratories|0.480|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.047|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-42|H-42|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361298|447816|-21.88780|64.50348|276||Borađ í nánast ţađ sama og í H-41 eđa um 4 m norđar. Bergiđ er breksíukennt ađ sjá (um 200 m hćđ). Blöđrulaust, mikiđ sprungukrađak mest undir 70° horni. |Sampled from near the same unit as H-41 or about 4 m further to the north. The rock appears to be brecciated (about 200 m elevation). Compact, cracked with veins mostly under 70°.|Lava flow|Flow-top breccia|Chlorite-epidote|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.500|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.040|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-43|H-43|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361294|447783|-21.88785|64.50318|285||Yfirborđ á hrauni. Hluti kjarnans er oxađur, ţeir eru mjög blöđróttir međ ljósgrćnum leir í blöđrum. Mjög blöđrótt og fyllt, margar sprungur, óreglulegar, ein ţeirra opin.|Lava surface. Part of the core is oxidized, rock is very vesicular with light green clay in the vesicles. Numerous filled vesicles, mineralized veins, irregular, some open veins.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.300|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.026|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-44|H-44|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361292|447773|-21.88788|64.50309|289||< 6 m ţykkt hraunlag, nćrri 50 cm ţykkum gangi. Bergiđ er smáblöđrótt. |Less than 6m thick lava flow, adjacent to a 50 cm thick dyke. Small vesicles. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.180|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories|3.85E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.54E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-45|H-45|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361284|447766|-21.88805|64.50302|295||Borađ í setlag milli fínkorna hraunlaga. Setlagiđ er lagskipt og fínkorna mjög (hćđ 210 m). Líklegast kargi, mjög blöđrótt, fyllt, ein sprunga 90° horna. |Sedimentary layer between fine-grained lavas. (210 m elevation). Likely a flow-top breccia, numerous filled vesicles, one vein 90° angle. |Lava flow|Flow-top breccia|Chlorite-epidote|2.72|Measured on crushed sample by Western Atlas Borehole Laboratories|0.980|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.097|He Gas pycnometry, Western Atlas Borehole Laboratories|5.73E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-46|H-46|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361278|447748|-21.88815|64.50286|302||Borađ er í ljósa ummyndun í breksíu nćrri yfirborđi hraunlags. Túffbreksía, porur fylltar. 1 sprunga undir 45° horni. |Light gray-green tuff, perhaps in a mixed layer clay zone, but within the smectite zone, influenced by a geothermal fissure, approx. 50 m from HG-2, by the river.|Lava flow|Flow-top breccia|Chlorite-epidote|2.68|Measured on crushed sample by Western Atlas Borehole Laboratories|0.410|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.022|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-47|H-47|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361278|447745|-21.88816|64.50283|303||Borađ í hraunlag, ţađ sama og H-46, og er 0.5-1.0 m neđan ţess. Bergiđ er fínkorna og enn nokkuđ breksíulegt. Bergiđ er mjög epidótríkt. Smáblöđrótt, jafnvel túffkennt, syllt. 3 sprungur undir 45-90° horni. |Lava flow, the same as H-46, and 0.5-1.0 m below. Rock is fine-grained and still quite brecciated. Rock is very epidote rich. Small vesicles, even tuff-like, 3 veins at a 45-90° angle.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.66|Measured on crushed sample by Western Atlas Borehole Laboratories|0.290|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.009|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-48|H-48|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361275|447739|-21.88820|64.50278|305||Borađ í epidótríka sónu í basalti, ţ.e. sama basalti og í H-47 en litlu neđar í lćknum. Líkist túffi, holufyllt, 2 sprungur undir 90° horni.|Basalt in an epidote rich zone in a basalt, approximately the same basalt as H-47 but a little closer to the lake. Looks like tuff, filled vesicles, two veins at a 90° angle.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.83|Measured on crushed sample by Western Atlas Borehole Laboratories|0.180|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.105|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-49|H-49|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361274|447740|-21.88823|64.50279|306||Borađ rétt ofan viđ neđri lagmót í 8 m ţykku plagíóklas dílóttu hraunlagi. Ţetta er rétt fyrir utan öskjujađarinn. Hćđarmćlir í 235 m. Smáblöđrótt og fyllt (einkum međ dökkum leir), ein óveruleg sprunga undir 90° horni.|Drilled in an 8 m thick lava layer with coarse-grained plagioclase. This is just outside the caldera margin. Altimeter at 235 m. Small filled-vesicles (appears to be with dark clay), one insignificant vein at a 90° angle.|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.92|Measured on crushed sample by Western Atlas Borehole Laboratories|0.250|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.009|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-50|H-50|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361272|447740|-21.88826|64.50279|306||Breksía neđan sýnis H-49 og er líklegast karginn úr hraunlaginu fyrir neđan. Nokkuđ blöđrótt fyllt, sprungukrađak, en mjög smáar, nema 2-3 sem viđast opnari nćrri yfirborđi.|Breccia below sample H-49 and is most likely the flow top breccia of underlying lava. Somewhat vesicular, with filled vesicles, fractured, but mostly small, except for 2-3 which appear to open towards the surface.|Lava flow|Flow-top breccia|Chlorite-epidote|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.160|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.010|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-51|H-51|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361272|447726|-21.88826|64.50266|310||Gulleit súr breksía í lćkjarfarvegi um 2-3 m innan viđ öskjujađarinn. Sýniđ mjög ósamleit. Smávegis ófyllt holrymi á staka stađ. Sprungunetskrađak undir mesmegnis 45° horni. Sumar viđast opnar viđ yfirborđ kjarnans. |Yellowish breccia in a stream channel about 2-3 m inside the caldera margin. Sample very inhomogenous. Slightly unfilled cavities in some places. Cracked at a maximum angle of 45°, some appear open at the surface of the core. |Silicic volcanic|Rhyolite tuff|Chlorite-epidote|2.66|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.102|He Gas pycnometry, Western Atlas Borehole Laboratories|1.76E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|6.91E-17|Measured by Western Atlas Borehole Laboratories|2.54E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-52|H-52|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361269|447709|-21.88831|64.50251|314||Fínkorna gangur á öskjujađri, mjög ummyndađur grágrćnn ađ lit. Blöđrulaust. 2 sprungur. |Fine-grained dyke at the edge of the caldera, very altered, gray-green in color. No obvious vesicles, two veins. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.410|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||9.87E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-53|H-53|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361267|447700|-21.88833|64.50243|317||Borađ í grófgerđa basaltbreksíu í lćkjarfarvegi ca. 30-40 m ofan og innan viđ kalderujađarinn. Mjög blöđrótt og fyllt, fjöldi óreglulegra sprungna. |Drilled in a coarse basalt breccia in a stream channel approx. 30-40 m above and inside the caldera margin. Numerous filled vesicles, numerous irregular veins. |Lava flow|Flow-top breccia|Chlorite-epidote|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.125|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.124|He Gas pycnometry, Western Atlas Borehole Laboratories|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-54|H-54|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361264|447695|-21.88838|64.50238|319||Súr breksía í lćkjarfarvegi ađeins ofan viđ kalderujađar, og ca. 100 m innan viđ kalderujađarinn (hćđ skv. hćđarmćli 270 m). Breksían er gulbrún og svört?, etv. Gefur epidótiđ ţessa ásýnd. Kjarnataka léleg. Ţétt smáblöđrótt og fyllt, fjöldi sprungna (ađ mestu fylltar epidóti). |Rhyolitic breccia in a stream channel just above the caldera margin, and approx. 100 m inside the caldera edge (height according to altimeter 270 m). Breccia is yellow-brown and dark? Possibly epidote in this sample. Sampling was difficult. Compact, small filled vesicles, numerous veins mostly filled with epidote. |Silicic volcanic|Rhyolite breccia|Chlorite-epidote|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.620|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.024|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-55|H-55|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361255|447686|-21.88856|64.50230|324||Súrt túff samlímt sem er mest í ţessari súru seríu (275m hćđ), sem sést í ofanverđu gilinu innan kalderunnar. Holufyllt túff, sterk 45°  sprungunet, 2 ţeirra drekka í sig vatn. |Rhyolitic tuff, consolidated which is the most in this acid series (275m height) and is seen in the upper gorge within the caldera. Filled vesicles, strong network of veins, 2 of which contain water. |Silicic volcanic|Rhyolite tuff|Chlorite-epidote|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.127|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.126|He Gas pycnometry, Western Atlas Borehole Laboratories|2.47E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.98E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-56|H-56|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361255|447686|-21.88856|64.50230|324||Líparít Ţar sem lagiđ sem borađ var í í H-55 breytist úr setkenndu efni í kristallađ ca. 10 m ofar. Stakar porur 90% fylltar, sprungukrađak. |Rhyolite  where the layer drilled in H-55 changes from sedimentary material to crystalline ca. 10 m above. Numerous pores, 90% filled, fractured. |Silicic volcanic|Rhyolite lava|Chlorite-epidote|2.69|Measured on crushed sample by Western Atlas Borehole Laboratories|0.141|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.140|He Gas pycnometry, Western Atlas Borehole Laboratories|2.17E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.95E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-57|H-57|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Flyđrunum í Hafnarfjalli|359840|447530|-21.91784|64.50032|243||Granófýr sýni tekiđ úr Flyđrunum í Hafnarfjalli úr hnullungi sem lá nćrri veginum. Bergiđ hart og ţess vegna tekinn hnullungur til borunar seinna. Bergiđ er mjög gropiđ, epidót í blöđrum, etv prímert? Nokkuđ smáblöđrótt og ófyllt. Engar sprungur. |Granophyre sample taken from Flyđrur i Hafnarfjall from a mound that is laying near the road. Rock is very hard and therefore a sample was taken for drilling back in the city. Rock is very porous, with epidote in vesicles, possibly primary? Somewhat small vesicles, with unfilled. No veins. |Silicic intrusion|Granophyre|Chlorite-epidote|2.63|Measured on crushed sample by Western Atlas Borehole Laboratories|0.650|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.064|He Gas pycnometry, Western Atlas Borehole Laboratories|2.02E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.65E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-58|H-58|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|354377|430328|-22.01434|64.34389|1||Borađur kjarni í 8-10 m  ţykkt dílótt basalt rétt neđan viđ brúna á Berjadalsá. í efsta hluta mesólít-skólesít belti. | 8-10 m thick porphyritic  basalt just below the bridge at Berjadalsá. In the upper part of the mesolite-scolesite zone.|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.190|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.008|He Gas pycnometry, Western Atlas Borehole Laboratories|3.16E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.75E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-59|H-59|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355732|428452|-21.98450|64.32765|53||Hraunlag ofar í ánni.  Um 1 m ţykkur breksíerađur toppur eđa botn á hraunlagi. Mjög zeólítíserađur (analsím og kabasít). Mjög blöđrótt og um 40% fyllt. A sýniđ er minna blöđrótt en önnur sýni međ sama númeri. 2 sprungur undir um 70° horni. |Lava flow further up river. About 1 m thick brecciated top or bottom of a lava flow. Numerous zeolites (analcime and chabazite). Very vesicular, about 40% filled. Sample is less vesicular than other samples with the same number. Two veins under 70° angle. |Lava flow|Flow-top breccia|Smectite-zeolite|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.315|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.313|He Gas pycnometry, Western Atlas Borehole Laboratories|4.75E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|4.18E-15|Measured by Western Atlas Borehole Laboratories|5.13E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-60|H-60|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355732|428445|-21.98449|64.32759|53||Flögótt dílótt basalt um 2-3 m ofar en H-59. Nćr blöđrulaust og sprungulaust. |Flow lineated porphyritic basalt about 2-3 m above H-59. Vesicles and fractures nearly absent.|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.89|Measured on crushed sample by Western Atlas Borehole Laboratories|0.420|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.038|He Gas pycnometry, Western Atlas Borehole Laboratories|6.91E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.09E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-61|H-61|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355749|428318|-21.98400|64.32646|58||Ţóleiít hraunlag um 8 m ţykkt, sýniđ tekiđ um 1 m ofan viđ botn lagsins og borađ samsíđa straumflögun. Bergiđ er fínkorna og ţétt. Gamall steptur vatnsveitustokkur neđan lagsins. Staksmáblöđrótt, fylltar međ dökkum leir, straumflögun er sterk, en engar sprungur sjást fylgja henni og sprungur sjást ekki.|Tholeiitic basalt flow about 8m thick, sample taken about 1 m above the bottom of the layer and drilled parallel to the flow banding. Rock is fine-grained and compact. An old water supply shaft below the layer. Few vesicles, filled with dark clay, flow-banding is strong, but no veins are visible. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-62|H-62|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355754|428313|-21.98391|64.32642|58||Sýni nćrri toppi sama ţóleiít hraunlags og H-61. Bergiđ smáblöđrótt. Karginn veđrađur í burtu af laginu. Borađ ţvert á straumflögun. Ath. H-61 feltmynd gerđ H-61 og 62. Smáblöđrótt, lerskán í blöđrum, ca. 40% fylltar (smćrri blöđrunar fylltar, ţćr stćrri allt niđur í 20%).|Sample near the top of the same tholeiitic basalt flow as H-61. Rock has small vesicles. Weathered flow-top breccia away from the layer. Note that a field picture is made of H-61 and H-62. Small vesicles, clay in vesicles, ca. 40% filled (smaller vesicles are filled, larger ones down to 20%). |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.290|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.015|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-63|H-63|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355794|428292|-21.98307|64.32624|63||Ţétt ţóleiít hraunlag 10-15 m ţykkt viđ hliđina á vatnsveitustíflunni. Borađ um 1 m frá botni lagsins. Borađ samsíđa straumflögun. Blöđrulaust, sterk straumflögun undir 90° horni, engar sprungur sjáanlegar sem fylgja straumflöguninni.|Compact tholeiitic lava flow 10-15 m thick next to the water supply dam. Drilled 1 m from the bottom of the layer. Drilled parallel to the flow-banding. Vesicles absent, strong flow-banding under 90° angle, no veins visible following the flow-banding. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Measured on crushed sample by Western Atlas Borehole Laboratories|0.700|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.003|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-64|H-64|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355803|428289|-21.98287|64.32622|64||Fínkorna ţóleiít hraunlag, nćrri toppi sama lags og H-63 er borađ í. Borađsamsíđa straumflögun, en hún er ekki áberandi í ţessu lagi. Feltmynd af afstöđu H-63 og 64. Blöđrulaust, veđrunarfletir í sýninu undir um 30° horni, 2 sprungur undir um 45° horni.|Fine-grained tholeiitic basalt lava flow, near the top of the same flow H-63 is drilled in. Drilled parallel to the flow-banding, which is not clearly visible in this layer. Field picture of H-63 and 64 are available. No vesicles, weathering surfaces in the sample under 30° angle, two veins at about 45° angle. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.84|Measured on crushed sample by Western Atlas Borehole Laboratories|0.170|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-65|H-65|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355764|428284|-21.98367|64.32616|59||Samlímt konglomerat. Stakar tómar blöđrur, ávöl bergkorn í ljósum millimassa.|Cemented conglomerate. Sparse empty vesicles, rounded granules in the light-colored ground mass. |Sediment|Sediment|Smectite-zeolite|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.141|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.137|He Gas pycnometry, Western Atlas Borehole Laboratories|1.92E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|1.97E-17|Measured by Western Atlas Borehole Laboratories|2.48E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-66|H-66|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358482|425907|-21.92526|64.30599|7||Setlag í fjörunni neđan og vestan viđ bćinn Innra-Hólm. Zeólítíserađ. Setiđ er fremur fínt (túffkennt?) međ stöku hnullungum. Sérstök ummyndun sem felst í áberandi ummyndunarsónum í kringum jarđhitaćđar. Sýni borađ í dökka hlutann og minna ummyndađa. |Sedimentary layer on the shore below and west of the town of Innra-Hólm. Zeolitized. The sediment is rather fine-grained (tuff-like) with occasional fragments. Drilled into a dark part with minimal alteration. Special alteration that consists of prominent alteration zones around geothermal veins. Sample drilled into the dark, less-altered part. |Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.44|Measured on crushed sample by Western Atlas Borehole Laboratories|0.180|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.177|He Gas pycnometry, Western Atlas Borehole Laboratories|1.18E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|1.48E-16|Measured by Western Atlas Borehole Laboratories|1.35E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-67|H-67|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358478|425906|-21.92526|64.05075|7||Kjarni úr ljósari hlutanum, og í sprunguummynduninni. Feltmynd af berútliti ásamt ljósmyndum. Móbergsset. Molar mjög túffkendir og setiđ óreglulegt ađ lit. Blöđrur smáar og virđast á miklu fylltar, 1 sprunga undir 90° horni.|Core from the lighter and more fractured part, and in the part with altered fractures.  Hyaloclastite sediment of tuffaceous origin, colour heterogeneous. Vesicles small and appear to be largely filled, 1 fracture with dip below 90°.|Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.70|Measured on crushed sample by Western Atlas Borehole Laboratories|0.275|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.222|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-68|H-68|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358452|425896|-21.92586|64.30589|7||Plagíóklas dílótt hraunlag um 4 m ţykkt og liggur ofan á setlaginu. Mjög zeólítaríkt en blöđrur ekki fylltar heldur meira húđ í blöđrunum. Kabasít, anasím, thompsonít og vottur af skólesíti, e.t.v. phillipsít. Stakblöđrótt >60% fylltar, engar sprungur sjáanlegar.|Plagioclase porphyritic basalt about 4m thick lying above the sedimentary layer. Very zeolite-rich but vesicles not filled rather more skin in vesicles. Chabazite, analcime, thompsonite, and traces of scolescite, along with others.|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.630|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.059|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-69|H-69|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358450|425893|-21.92590|64.30586|7||Tekiđ um 30 cm ofar í sama hraunlagi og H-68. Sýniđ er mun blöđróttara. Mjög blöđrótt og minnstu blöđrur alveg fylltar (zeólítar) ţćr stćrri >20%, engar sprungur sjáanlegar.|About 30 cm above the same lava flow as H-68. Sample is much more vesicular. Very vesicular and the smallest vesicles completely filled (zeolites) whereas the largest >20%, no visible veins. |Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.540|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.048|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-70|H-70|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358446|425886|-21.92596|64.30580|6||Tekiđ vestar í sama lagi og H-68 og 69. Mjög blöđrótt og zeólítíserađ neđra borđ hraunlagsins um 30 cm ofan lagmótanna. Mjög blöđrótt, analsím í blöđrum ca 40% fylltar, minni blöđrur fylltar en ţćr stćrri minna fylltar, 3 sprungur, ţar af ein opin viđ kjarnayfirborđ. |Taken to the west in the same layer as H-68 and H-69. Very vesicular and zeolitized lower surface of the lava layer about 30 cm above the layer boundary. Very vesicular, analcime in vesicles ca 40% filled, smaller vesicles filled but the largest less filled, 3 veins, one of which opens into the surface of the core. |Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.960|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.093|He Gas pycnometry, Western Atlas Borehole Laboratories|1.65E-14|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|8.96E-15|Measured by Western Atlas Borehole Laboratories|1.83E-14|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-71|H-71|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Kúludalsá to the south of Akrafjall|361654|427586|-21.86135|64.32234|23||Dílótt basalt vestan viđ ósa árinnar. Mesólít-skólesít belti. Borađ í ţétt berg. Karginn er óreglulegur ţar sem sýniđ er tekiđ. Ađ ţví virđist blöđrulaust, 3 sprungur undir um 70° horni. (Yfirleitt eru sprungur í kjarnanum taldar međ hringferđ um 2 cm kjarnabút og ţeirra tölu deilt međ 2).  |Porphyritic basalt to the west of the river estuary. Mesolite-scolesite zone. Drilled into dense rock. Flow-top breccia is irregular where the sample is taken. Seemingly vesicle-free, three veins with a 70° dip. (Usually cracks in the core are counted with a diameter of 2 cm core fragment and their number divided by 2).|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|3.00|Measured on crushed sample by Western Atlas Borehole Laboratories|0.410|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.038|He Gas pycnometry, Western Atlas Borehole Laboratories|3.55E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|9.87E-17|Measured by Western Atlas Borehole Laboratories|4.84E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-72|H-72|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Kúludalsá to the south of Akrafjall|361644|427577|-21.86155|64.32226|23||Hraunlagiđ ofan H-71 og vestan. 6-8 m ţykkt dílótt eins og síđasta sýni. Nokkuđ smáblöđrótt og fylltar međ dökkum leir, sprungulaust. Stór blađra (1 cm) ađeins 30% fyllt.|Lava flow above and to the west of H-71. 6-8 m thick porphyritic basalt like the previous sample. Some small vesicles and filled with dark clay, vein-free. Large vesicle (1 cm) only 30% filled. |Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.390|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.033|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-73|H-73|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Ferro-alloy plant in Grundartangi|365273|430685|-21.78942|64.35157|5||Basaltlag niđri í fjöru beint fyrir neđan verksmiđjuna. Stórblöđrótt plagíóklas dílótt líklegt ţóleiít í skólesít-mesólítbelti. Stakblöđrótt ađ mestu fylltar, 3 sprungur međ 90°. Sterk straumflögun (ţóleiítleg) undir 0° horni.|Basalt flow on the beach directly below the factory. Large vesicles, plagioclase porphyry likely tholeiite in scolescite-mesolite belt. Large vesicles mostly filled, 3 vesicles with 90°. Strongly flow-banded (ţóleiítleg) with a 0° dip.|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.99|Measured on crushed sample by Western Atlas Borehole Laboratories|0.360|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.019|He Gas pycnometry, Western Atlas Borehole Laboratories|3.16E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.85E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-74|H-74|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akranes, between the lighthouses on Skipaskagi|350289|426546|-22.09500|64.30823|0||Ólivín ţóleiít hraunlag. Sýniđ tekiđ á klöpp á milli vitanna á Skipaskaga. Hraunlögin líklega innan dyngju. Međ dökkri leirskán, sprungulaust. |Olivine tholeiite basalt flow. Drilled into the upper part of a rock between the lighthouses on Skipaskagi. Lava flow likely part of a shield volcano. With dark clay alteration, without fractures.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.250|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.024|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-75|H-75|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|Akranes, between the lighthouses on Skipaskagi|350268|426592|-22.09547|64.30862|0||Borađ ofan í ólivín ţóleiít hraun viđ nýja vitann. Samskonar hraun og H-74. Stakblöđrótt, 60% fyllt, 2 sprungur.|Drilled into the olivine tholeiite lava at the new lighthouse. Same lava as H-74. vesicle filling ca. 60% filled, 2 fractures.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.91|Measured on crushed sample by Western Atlas Borehole Laboratories|0.130|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.011|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-76|H-76|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|To the S/SE of the old HB fish processing factory in Akranes|350408|426635|-22.09263|64.30908|0||Borađ í sama berg nćr suđur eđa suđaustan viđ skreiđarhjalla HB. 1 fyllt blađra, sprungulaust. |Lava to the S/SE of the old HB fish processing factory. 1 filled vesicle, vein-free.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.97|Measured on crushed sample by Western Atlas Borehole Laboratories|0.230|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.013|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-77|H-77|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|To the S/SE of the old HB fish processing factory in Akranes|350414|426630|-22.09250|64.30904|0||Fćrt sig um 5 m í átt ađ sjónum og borađ í sama lag en mun blöđróttara en H-76. 2 smáar blöđrur, 2 sprungur undir 0° horni. |Above 5m closer to the sea as H-76 and drilled into the same layer as H-76 but much more vesicular. 2 small vesicles, 2 veins with a 0° dip. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.330|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.025|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-78|H-78|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|The beach to the east of Ytrihólmur|353410|425745|-22.02977|64.30240|3||Ólivín ţóleiít basalt úr dyngju. Grófkorna ólivín ţóleiít, blöđrulaust, sprungulaust.|Olive tholeiite basalt from a shield volcano. Coarse-grained olivine tholeiite, vesicle-free, vein-free. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.95|Measured on crushed sample by Western Atlas Borehole Laboratories|0.540|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.053|He Gas pycnometry, Western Atlas Borehole Laboratories|2.66E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.45E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-79|H-79|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|The beach to the east of Ytrihólmur|353574|425741|-22.02638|64.30244|4||Dyngjubasalt, grófkorna, um 50 m austar borađ í fremur ţéttan hluta lags. Blöđrulaust, 1 sprunga undir um 90° horni. |Coarse-grained basalt from a shield volcano, about 50 m east of H-78 in a dense part of the flow. Vesicle-free, 1 vein with a dip of about 90°.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.97|Measured on crushed sample by Western Atlas Borehole Laboratories|0.730|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.072|He Gas pycnometry, Western Atlas Borehole Laboratories|2.57E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|3.95E-17|Measured by Geological Survey of Denmark and Greenland|1.64E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_H-80|H-80|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|28.8.1992|Surface|The beach to the east of Ytrihólmur|353594|425752|-22.02599|64.30254|5||Dyngjubasalt, sama og síđasta sýni nema blöđróttara. Ca, 10 m austan viđ H-79. Nćr blöđrulaust, grófkorna ólivín ţóleiít, mögulegar 2-3 sprungur undir 20° horni.|Shield volcano basalt, same as H-79 except vesicular. Approximately 10 m east of H-79. Nearly vesicle-free, coarse-grained olivine tholeiite, possibly 2-3 veins with a 20° dip.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.94|Measured on crushed sample by Western Atlas Borehole Laboratories|0.490|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.046|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_H-81|H-81|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the north side of the mine|382857|434487|-21.42877|64.39215|28||Rhyolít. Líparít kubbabergsbólstri, sýni tekiđ úr miđju stuđuls. Ummyndun óljós í felti og var ţví látiđ bíđa eftir XRD á leir. |Rhyolite. Liparite cube-jointed basalt, sample taken from the center of the column. Alteration unclear in the field and was left to be analyzed with XRD. |Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.30|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.056|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.16E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.63E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-82|H-82|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the north side of the mine|382795|434482|-21.43004|64.39208|27||Líparít breksía. Sýni tekiđ úr steini viđ ána, norđan viđ námuna. XRD - leir -> smektít|Rhyolite breccia. Sample taken from a stone by the river, north of the mine. XRD suggests clay is smectite. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.242|He Gas pycnometry, Geological Survey of Denmark and Greenland|5.88E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|1.40E-16|Measured by Geological Survey of Denmark and Greenland|6.11E-15|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-83|H-83|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the north side of the mine|382861|434489|-21.42868|64.39217|29||Rhyolít-kubbaberg? Súlfíđsóna í sama líparíti og á undan í sprungusónu. Bergiđ er glerkennt.|Rhyolite cube-jointed? Sulfide zone in the same liparite as before in the crack zone. Rock is glassy. |Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.28|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.015|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.18E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.27E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-84|H-84|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the north side of the mine|382861|434489|-21.42868|64.39217|29||Rhyólít. Sami ţursabergseitill og á undan sýni tekiđ um 4 m frá H-83 ađ ţví er virđist í ferskari hlutanum. Kubbabergseitlarnir eru 10-20 m langir og ca. 4-6 m háir (ónákvćmt). |Rhyolite. The same cube-jointed basalt as before the sample taken about 4 m from H-83 apparently in the less altered part. The cube-jointed units are 10-20 m long and approx. 4-6 m high (inexact).|Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.39|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.072|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.73E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|5.92E-18|Measured by Geological Survey of Denmark and Greenland|2.83E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-85|H-85|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the north side of the mine|382857|434501|-21.42878|64.39228|31||Rhyolíttúff. Blöđrótt fremur hart berg og eru blöđrur tómar. Ath. H-81-85 eru tekin ađ norđanverđu í námunni.|Rhyolite tuff. Vesicular, rather hard rock, but vesicles are empty. Note that H-81 to 85 are taken from the north side of the quarry. |Silicic volcanic|Rhyolite tuff|Smectite-zeolite||Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.000|||||||||||||||||||||||||
OS-95017_H-86|H-86|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hvalfjörđur, Líparite quarry, on the south side of the mine|382857|434501|-21.42878|64.39228|31||Rhyolíttúff. Sýni tekiđ í sunnanverđri námunni í mjög ummynduđu og sprungufylttu túffi.|Rhyolite tuff, taken from the south side of the quarry in very altered tuff with filled veins. |Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.24|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.186|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.57E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.64E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-87|H-87|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382881|435448|-21.42903|64.40077|97||Rhyolítbreksía, ţ.e. súrt túff međ líparít og biksteinsbrotum í. Ummyndun en kabasít sést í blöđrum. (XRD - leir -> smektít).|Rhyolite breccia, i.e. Acid tuff with liparite and bitumen fragments in it. Chabazite alteration visible in vesicles (XRD - clay -> smectite)|Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.23|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.183|He Gas pycnometry, Geological Survey of Denmark and Greenland (2 measurements) and Western Atlas Borehole Measurements|1.74E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|9.87E-19|Measured by Geological Survey of Denmark and Greenland|2.96E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-88|H-88|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382890|435442|-21.42883|64.40072|97||Líparít eđa rhyolít. Ljós drappleitt berg nokkuđ ţétt eđa massíft. Ath. Sýni tekiđ úr hnullungum eftir spregingar í námunni.|Liparite or rhyolite, Light dripping rock fairly dense or solid. Note that samples taken from piles after cracking in the quarry. |Silicic intrusion|Rhyolite dyke|Smectite-zeolite|2.20|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)|||0.186|He Gas pycnometry|1.70E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|8.88E-18|Measured by Geological Survey of Denmark and Greenland|2.94E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-89|H-89|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382897|435439|-21.42870|64.40069|96||Líparít eđa rhyolít. Sýni tekiđ úr ljósgrábrúnu fínkorna ţéttu bergi. Ummyndun? Borađ í bergstáliđ í námunni. |Liparite or rhyolite, sample taken from light gray-brown fine-grained dense rock. Alteration? Drilled into rock cliff in the quarry.|Silicic intrusion|Rhyolite dyke|Smectite-zeolite|2.22|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.206|He Gas pycnometry, Western Atlas Borehole Laboratories|6.91E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.28E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-90|H-90|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|The beach in Hvalfjörđur, near the village of Hrafnabjörg|378465|434913|-21.52008|64.39442|19||Dólerít, á Hvalfjarđarströnd í námu. Sýni af nokkuđ ferklegu bergi.|Dolerite, on the Hvalfjörđur coast in a quarry. Sample of fairly fresh rock. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.98|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.005|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-91|H-91|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|The beach in Hvalfjörđur, near the village of Hrafnabjörg|378455|434905|-21.52028|64.39435|19||Dólerít, u.ţ.b. 20 cm sprungubelti í gegnum dólerítiđ. Ummyndun er nokkuđ viđ sprungubeltiđ og sjást m.a. kvars, kalsít og pýrít. (XRD - leir -> smektít)|Dolerite, approximately 20 cm thick belt of fractures through the dolerite. There is some alteration in the fractured area with quartz, calcite, and pyrite (XRD - clay -> smectite)|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|||||0.000|||||||||||||||||||||||||
OS-95017_H-92|H-92|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Rock quarry to the west of Hafnarfjall|358491|446800|-21.94516|64.49322|37||Gangberg, fínkorna keilugangur, sem sker dílótt fínkorna basaltlag or er epidót í basaltinu. |Fine-grained cone sheet cutting a fine-grained basalt layer, with epidote in the basalt.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.97|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.022|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-93|H-93|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Rock quarry to the west of Hafnarfjall|358494|446795|-21.94510|64.49317|37||Basalthraun, fínkorna smáplagíóklasdílótt basaltlag. Sýni tekiđ úr ferskari hluta lagsins, en ţađ er >6m á ţykkt.|Basalt lava, a fine-grained porphyritic basalt lava flow. Sample taken from the fresher part of the layer, which is >6 m thick.|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.93|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.004|He Gas pycnometry, Geological Survey of Denmark and Greenland|4.93E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||9.87E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-94|H-94|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Rock quarry to the west of Hafnarfjall|358497|446794|-21.94503|64.49316|38||Basalthraun, sama hraunlag og H-93, en nú var sýni tekiđ úr ummynduđum grćnleitum hluta lagsins. Bćđi sýnin eru tekin um 0.5 m ofan viđ keiluganginn (H-92).|Basalt lava, the same lava flow as H-93, but now a sample was taken from the more altered greenish part of the layer. Both samples are taken about 0.5 m above a cone dyke (H-92).|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.85|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.045|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-95|H-95|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362439|448596|-21.86481|64.51093|182||Berggangur 1,5 m ţykkur af ţóleiítgerđ, dílóttur. Strik 10° og halli 25° til austurs. Nokkuđ um fínar óreglulegar kristallađar ćđar. Sýnatökustađur rétt neđan stíflu vatnsveitu Borgarness. |Dyke, 1.5 m thick, tholeiitic, porphyritic. Strike 10 deg and dips 25 degrees to the east. Some fine irregular crystallized veins. Sampling site just below Borganes water supply dam.|Basaltic intrusion|Porphyritic basaltic intrusion|Chlorite-epidote|2.95|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.015|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.83E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|7.80E-17|Measured by Geological Survey of Denmark and Greenland|2.55E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-96|H-96|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362440|448610|-21.86480|64.51106|184||Súrt túff í árfarveginum ca. 20 m frá H-95. |Rhyolitic tuff in the river channel approx. 20 m from H-95.|Silicic volcanic|Rhyolite tuff|Chlorite-epidote|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.183|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.55E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-97|H-97|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362418|448618|-21.86526|64.51112|179||Gangberg, bergiđ er međalkorna ţétt nokkuđ ummyndađ basalt. Stefna 56° og er lóđrétt. XRD -> Leir -> smektít/blandlag. Aldursröđ: H-99> H-98>H-97|Dyke, medium-grained, dense, fairly altered basalt. Strike 56° and it is horizontal. XRD - clay -> smectite/mixed-layer. Age relationships: H-99>H-98>H-97.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)|||0.016|He Gas pycnometry, Geological Survey of Denmark and Greenland (4 measurements) and Western Atlas Borehole Laboratories (1 measurement)|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.95E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-98|H-98|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362420|448618|-21.86522|64.51112|179||Keilugangur mjög sprunginn og virđist ummyndađri heldur en H-99. Strik 350°. Gerđur úr ólvín-ţóleiít. |Cone-sheet, very fractured, more altered than H-99. Strike 350°. Made of olivine tholeiite. |Basaltic intrusion|Porphyritic basaltic intrusion|Mixed-layer clay|2.91|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.128|He Gas pycnometry, Geological Survey of Denmark and Greenland|6.91E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.38E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-99|H-99|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362423|448616|-21.86517|64.51111|180||Gangberg. Basaltkeilugangur dílóttur, 1,5 m á ţykkt mjög svipađur og H-95. Strik 350°. |Intrusion, basaltic cone sheet, porphyritic, 1.5 m thick, very similar to H-95. Strike 350°.|Basaltic intrusion|Porphyritic basaltic intrusion|Mixed-layer clay|2.94|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.009|He Gas pycnometry, Geological Survey of Denmark and Greenland||||||||||||||||||||||||
OS-95017_H-100|H-100|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362440|448610|-21.86480|64.51106|184||Basalt keilugangur um 1 m á ţykkt, mjög ummyndađur. Strik er um 6°. |Basaltic cone sheet, approx. 1 m thick, very altered. Strike is about 6°.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|2.77|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.108|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-101|H-101|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362713|447506|-21.85809|64.50127|334||Innst í innra-seleyrargili í grasserandi epidót-amfiból belti á öskjujađri. Innskot um 100%. Strik 170° og halli 60°. Basaltgangur. Um 0,5 m fínkornóttur laggangur, smásprunginn. Sýni tekiđ úr jađrinum. |Inside of inner-seleyrargil in epidote-amphibole alteration zone on the margin of the caldera. Intrusion density about 100%. Strike 170° and dip 60°. Basaltic dyke, about 0.5 m fine-grained flow, micro-fractured. Sample taken from perimeter. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.86|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.038|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-102|H-102|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362702|447486|-21.85829|64.50109|340||Gangberg (silla) fínkorna holufyllt ţéttsprungiđ ţóleiít basalt. Um 1 m á ţykkt. |Sill, fine-grained, filled-vesicles, densely fractured tholeiitic basalt. About 1  m thick. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.015|He Gas pycnometry, Geological Survey of Denmark and Greenland||||||||||||||||||||||||
OS-95017_H-103|H-103|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362694|447466|-21.85844|64.50091|346||Gangberg (silla) fínkorna blöđrótt ţóleiít basalt, sem liggur ofan á H-102 og er um 1 m á ţykkt. |Sill, fine-grained, vesicular tholeiitic basalt, that lies above H-102 and is about 1 m thick.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.83|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.025|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-104|H-104|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362691|447459|-21.85850|64.50084|348||Líparít innskot, óreglulegt á eđa viđ öskjujađarinn líklega um 1m á ţykkt. Litur gulur og rauđgulur og blöđrur sjást í ţví. |Rhyolite dyke, irregular at or near the edge of the caldera, probably about 1m thick. Yellow or reddish-yellow in color, with visible vesicles. |Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.178|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.04E-15|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|4.72E-16|Measured by Geological Survey of Denmark and Greenland|1.46E-15|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-105|H-105|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Inner Seleyrargil, by the creek in the gorge|362689|447451|-21.85854|64.50078|350||Berggangur, basaltkeilugangur 0,5 - 1 m á ţykkt og er dílóttur. Er viđ lćkinn í gilinu rétt viđ H-101 - 103 og er samsíđa ţeim. Stefna og halli 50° og 50°.|Basaltic cone sheet approx. 0.5-1 m thick and porphyritic. Is by the creek in the gorge right by H-101-103 and is parallel to them. Strike and dip 50° and 50°.|Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.91|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.022|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||8.88E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-106|H-106|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Innra-Seleyrargil, by the waterfall on the west side where the gorge splits|362658|447893|-21.85959|64.50472|254||Gangberg, langsprunginn fínkorna smádílóttur basaltgangur. Zeólítar sjást í langsprungum og einnig korsnnet af fínum sprungum. Ţykkt 50 cm. Stefna 20° og er lóđréttur. Sýnatökustađur er viđ fossinn vestan meginn, ţar sem giliđ klofnar. |Long, fine-grained, finely porphyritic basaltic dike. Zeolites visible in longitudinal veins and also in a network of fine cracks. Thickness 50 cm. Strike 20°. Sampling point is by the waterfall on the west side, where the gorge splits. |Basaltic intrusion|Porphyritic basaltic intrusion|Epidote-actinolite|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.166|He Gas pycnometry, Geological Survey of Denmark and Greenland|5.13E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.15E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-107|H-107|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|9.9.1993|Surface|Innra-Seleyrargil, by the waterfall on the west side where the gorge splits|362658|447893|-21.85959|64.50472|254||Basaltbreksía. Hér er um ađ rćđa grannberg milli keiluganga eđa misgengisbreksía, ljósgrá á lit og súlfíđrík, u.ţ.bţ 0.5 m á ţykkt. Er viđ fossinn rétt neđan viđ H-106. |Basaltic breccia. Neighboring rock to cone sheets or fault breccia, light-green due to alteration, with filled vesicles. Located by the waterfall just below H-106. |Lava flow|Flow-top breccia|Epidote-actinolite|2.83|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.214|He Gas pycnometry, Geological Survey of Denmark and Greenland|6.58E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.58E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-108|H-108|Guđmundsson et al., 1995|Guđmundsson et al., 1995|9.9.1993|Surface|Inner Seleyrargil|362658|447882|-21.85958|64.50463|257||Basalthraun. Efri hluti hraunlags fín-međalkorna líklega ţóleiít basalt. Bergiđ er ljós grćnt af ummyndun, holufyllt og blöđrótt. Pýrít og amfiból sjást. Sýnatökustađur ca. 20 m frá H-107. Teknir voru sérkjarnar af sprungufyllingum, dökkgrćnir og hvítir.|Basaltic lava. The upper part of the lava layer is fine-medium grained and probably tholeiitic. The rock is light green due to alteration, and vesicular. Pyrite and amphibole are seen. Sampling point approx. 20 m from H-107. Special cores of crack fillings were taken, dark green and white.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.093|He Gas pycnometry, Geological Survey of Denmark and Greenland|4.64E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|5.92E-18|Measured by Geological Survey of Denmark and Greenland|4.65E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-109|H-109|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362658|447870|-21.85957|64.50452|259||Basalthraun, tekiđ úr miđhluta ţess um ţađ bil 20 m frá H-108. Bergiđ er fín-međalkorna og blöđrótt.|Basaltic lava, taken from the central part about 20 m from H-108. Sample is fine-medium grained and vesicular.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.049|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.43E-16|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|9.87E-19|Measured by Geological Survey of Denmark and Greenland|2.93E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-110|H-110|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362661|448034|-21.85967|64.50599|223||Blöđrótti hluti basaltlags, ţ.e. á mótum tveggja basalthrauna. Erfitt er ađ dćma um ţykkt laganna ţar sem ekki sést í botn né topp ţeirra vegna skriđu og innskota. Sýnatökustađur um 4 m frá H-109. Pýrít sést og er mikiđ af ţví. Annars er bergiđ grćnleitt vegna ummyndunar. |Vesicular part of a basaltic lava flow taken at the boundary of two lava flows. Sampling point about 4 m from H-109. It is difficult to judge the thickness of the layers as they are not visible at the bottom or top due to scree and intrusions. Abundant pyrite. Otherwise the rock is greenish due to alteration.|Lava flow|Medium-coarse grained basaltic lava|Epidote-actinolite|2.84|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.112|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.95E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-111|H-111|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362662|448027|-21.85964|64.50593|225||Basalthraunlag, frekar ţétt og međalkorna og virđist klórítríkt. Stađsetning er beint fyrir neđan hnitapunkt H-101. |Basalt lava layer, rather compact and medium-grained and appears chlorite-rich. Location is right behind the coordinate point H-101.|Lava flow|Medium-coarse grained basaltic lava|Epidote-actinolite|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.022|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-112|H-112|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362663|448013|-21.85960|64.50580|229||Basalthraun um miđbik hraunlagsins 1-2 m neđan viđ laggang (sillu). |Basalt lava in the middle of the flow, 1-2 m below a horizontal intrusion (sill). |Lava flow|Medium-coarse grained basaltic lava|Epidote-actinolite|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.049|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-113|H-113|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362662|448006|-21.85962|64.50574|230||Basalthraun ofan viđ lagganginn í blöđróttari hlutanum nálćgt toppinum á laginu. |Basaltic lava above the sill in a more vesicular part near the top of the layer.|Lava flow|Medium-coarse grained basaltic lava|Epidote-actinolite|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.030|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-114|H-114|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362671|447973|-21.85939|64.50545|241||Súr laggangur. Sýniđ er tekiđ í lćknum og er greinilegt ađ mikil ummyndun fylgir honum. Strik er 145° og halli 10° til austurs. Ath H-108 er ca 11m ofan viđ súra kontaktinn. |Rhyolitic sill. Sample is taken in the lake and is notably altered. Strike is 145° and dip 10° to the east. Note that sample H-108 is ca. 11 m above the acid contact. |Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.140|He Gas pycnometry, Geological Survey of Denmark and Greenland|8.88E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.78E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-115|H-115|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362673|447967|-21.85936|64.50539|243||Basaltgangur eins meters ţykkur. Gangurinn óreglulegur og sker súra innskotiđ (H-114) og er ţéttur af sprungufyllingum. Pýrít er algengt (ath. Eldri ummyndun en sú súra). Erfitt ađ mćla strik innskotsins en ţađ gćti veriđ 10°. |Basaltic dyke, approx 1 m thick. The dyke is irregular and cuts the rhyolitic intrusion (H-114) and is dense with filled veins. Pyrite is abundant (note an older alteration than the acidic). Difficult to measure the strike of the intrusion but it could be 10°.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.012|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-116|H-116|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362671|447968|-21.85939|64.50540|242||Basaltkeilugangur um 1 m á ţykkt og er fínkorna. Sýni tekđ úr miđju hans. Strik 305° of halli 35° til austurs. |Basaltic cone sheet approx. 1 m thick. Fine-grained. Sample taken from the middle. Strike 305° and dip 35° to the east.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.005|He Gas pycnometry, Geological Survey of Denmark and Greenland|5.92E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.09E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-117|H-117|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362670|447956|-21.85941|64.50529|244||Basaltkeilugangur um 1,5 m á ţykkt og er fínkorna. Stilbítsprunga sést ofan viđ ganginn. Sýni tekđ úr miđju hans. Strik 305° og halli 35° til austurs. |Basaltic cone sheet approx. 1.5 m thick and fine-grained. Stilbite veins can be seen on the top of the dyke. Sample taken from the middle. Strike 305° and dip 35° to the east.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.84|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.040|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-118|H-118|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362666|447939|-21.85947|64.50514|247||Basalthraun. Mjög blöđrótt fínkorna basalt, sennilega toppur á hraunlagi. Ummyndun getur veriđ tengd órelulegum basaltgangi 2-3 m ţykkum. Epidót er algengt og blöđrur eru leirfylltar. Í um 20 cm fjarlćgđ frá ganginum. |Basaltic lava, very vesicular fine-grained basalt, likely the top of the lava flow. Alteration could be connected with the irregular basaltic dykes 2-3 m thick. Epidote is abundant and vesicles are clay filled. At a approx. 20 cm distance from the dyke.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.037|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-119|H-119|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362695|447753|-21.85869|64.50349|287||Basaltgangur, sem nefndur er í lýsingu H-118, sprunginn og ummyndađur.|Basaltic dyke, which is referred to in the description for H-118, fractured and altered. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.072|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.97E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-120|H-120|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362688|447752|-21.85883|64.50347|287||Basalthraun. Toppur á mjög blöđróttu hraunlagi í árfarveginum. Stađurinn var rétt ofan viđ sveig á gilinu, ţar sem lítill foss er. Ath. Toppurinn á hraunlaginu er í árfarveginum og eru ţví engar upplýsingar um ţykkt lagsins, en lögin ofan viđ eru 6-8 m ţykk.|Basaltic lava, top of a very vesicular lava flow in the river channel. The sampling point was just above the bend in the gorge, where there is a small waterfall. Note that the top of the lava layer is in the river channel and therefore it is not possible to measure the thickness of the layer, but the overlying layers are 6-8 m thick.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.022|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-121|H-121|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362682|447732|-21.85895|64.50329|291||Basalthraun á sama stađ og H-120, en fjćr ummyndunarsónu viđ sprungurnar. Bergiđ virđist vera nokkuđ ţétt, ţ.e. fínkorna smáblöđrótt. Klórít ađ mestu í blöđrum og ţađ er međ epidót í sprungum og ef til vill amfiból. |Basaltic lava from the same place as H-120, but away from the alteration zone with fractures. The rock appears to be somewhat compact, i.e. fine-grained with small vesicles. Chlorite dominates in the vesicles with epidote in veins (perhaps amphibole).|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.79|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.003|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-122|H-122|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362686|447564|-21.85871|64.50179|328||Basalthraunlag fínkorna og smáblöđrótt, mjög ummyndađ ţóleiít. Bergiđ er grćnt - ljósgrćnt á lít og sjást epidót, klórít, ef til vill granat (brúnleitur) ásamt hvítum torkennilegum útfellingum. Sýni tekiđ á stalli viđ svigđu í um 280 m hćđ skv. Hćđamćli.|Basaltic lava, fine-grained and finely vesicular, very altered tholeiite. The rock is green - light green with apparent epidote, chlorite and perhaps garnet (brown-colored) as well as difficult to make out white precipates. Sample taken at a ledge at a bend in the road at about 280 m elevation according to the altimeter.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.88|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.045|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-123|H-123|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362692|447574|-21.85858|64.50187|325||Basalthraun, fínkorna af ţóleiít gerđ grágrćnt á lit. Sýni sennilega úr miđbiki lagsins, viđ hliđina á H-122, en ca. 1m ofar. |Basaltic lava, fine-grained, grey-green in color. Sample probably from the middle of the layer, next to H-122 but approx. 1 m above.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.95|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.034|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-124|H-124|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362648|448073|-21.85997|64.50633|210||Dólerítgangur 3 m ţykkur grófkorna basalt sambćrilegur viđ fasa 12 í Geitafelli. Hćđarmćlir sýnir 210 m á sýnatökustađ. Stefna 28° og halli 28° til austurs. |Doleritic dyke, 3 m thick, coarse-grained basalt comparable to phase 12 in Geitafell. Altimeter shows 210 m at the sampling point.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.027|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-125|H-125|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362650|448061|-21.85992|64.50622|210||Dólerítgangur, sá sami og H-124 og nú úr miđju hans. |Doleritic dyke, similar to H-124 but in the middle. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.88|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.079|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.88E-17|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.45E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-126|H-126|Guđmundsson et al., 1995|Sigurđsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362645|448064|-21.86002|64.50625|208||Basalthraun, fínkorna smáblöđrótt og ummyndun líklega í smektít beltinu. Sýnatökustađur skammt frá H-124 - 125. |Basaltic lava, fine-grained, micro vesicular and altered likely in the smectite zone. Sampling spot not far from H-124-125. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.74|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.046|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||3.95E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-127|H-127|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365816|449959|-21.79584|64.52450|47||Basalthraun,  fínkorna og ţétt ţóleiítbasalt. Lagiđ er 8-10 m ţykkt. Sýnataka  í mynni gilsins ađ sunnan.|Basaltic lava, fine-grained and dense tholeiitic basalt. Layer is 8-10 m thick. Sample was taken at the mouth of the gorge to the south. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.017|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-128|H-128|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365865|449940|-21.79479|64.52435|52||Basalthraunlag, sýni tekiđ úr blöđróttum toppi sama hraunlags og H-128. |Basaltic lava, sample taken from the vesicular top of the same lava flow as H-128.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.079|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-129|H-129|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365870|449922|-21.79467|64.52419|53||Líparít. Sýnatökustađur viđ botninn á neđsta líparítlaginu í Árdalsgili. Bergiđ er hnúđótt og eru ţeir frekar massífir annars stađar var nánast vonlaust ađ ná sýnum. |Rhyolite. Sampling point at the bottom of the bottom layer of liparite in Árdalsgil. The rock is lumpy and it was rather difficult to take a sample in other places.|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.33|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.041|He Gas pycnometry, Geological Survey of Denmark and Greenland|7.90E-18|Measured by Western Atlas Borehole Laboratories, CMS-300 device, helium gas, Klinkenberg and Forcheimer corrections included|||1.58E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-130|H-130|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365867|449907|-21.79472|64.52406|54||Líparít. Sýni tekiđ um miđbik í fyrsta líparítlaginu í Árdalsgili sama og H-129 |Rhyolite. Samples taken in the middle of the first rhyolite layer in Árdalsgil, the same as H-129|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.140|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.46E-17|Measured by Geological Survey of Denmark and Greenland|1.09E-17|Measured by Geological Survey of Denmark and Greenland|2.54E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-131|H-131|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365927|449781|-21.79335|64.52295|65||Basaltgangur, keilugangur 1,5 m ţykkur fín-međalkorna. Svipađur stađur og H-130. |Basaltic  cone sheet, 1.5 m thick fine-medium grain. Similar place as H-130.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.93|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.044|He Gas pycnometry, Geological Survey of Denmark and Greenland (3 measurements) and Western Atlas Borehole Laboratories|3.91E-17|Measured by Geological Survey of Denmark and Greenland|||6.78E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-132|H-132|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365956|449748|-21.79272|64.52267|70||Líparít. Sýni tekiđ í flúđum í ánni og úr efri hluta sama lags og á undan. Bergiđ er straumflögótt. |Rhyolite. Samples taken near the river and from the upper part of the same layer as before.|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.31|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.044|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.95E-16|Measured by Geological Survey of Denmark and Greenland|||2.80E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-133|H-133|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365960|449756|-21.79265|64.52274|69||Líparít. Sýni tekiđ úr toppinum á líparítlaginu hér á undan međ breksíulegt útlit en ţétt og var sýnatökustađurinn úr eins konar biksteinshrúgaldi. |Liparite. Sample taken from the top of the above-mentioned liparite layer with brecciated appearance and compact. The sampling point was a kind of pitch-stone heap.|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.31|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.043|He Gas pycnometry, Geological Survey of Denmark and Greenland||||||||||||||||||||||||
OS-95017_H-134|H-134|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365959|449753|-21.79267|64.52272|69||Rhyolít, sýni tekiđ viđ hliđina á H-133 í eins konar millimassa. |Rhyolite, sample taken next to H-133 in a kind of groundmass.|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.39|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.077|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.55E-17|Measured by Geological Survey of Denmark and Greenland|||6.32E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-135|H-135|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|365960|449750|-21.79263|64.52269|70||Súrt túff, ljósgrćnt á lit og situr í bollum efst í líparítlaginu. Á sama stađ og H-133-134. |Acidic tuff, light green in color and sitting at the top of the rhyolite layer. At the same place as H-133-134.|Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.31|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.185|He Gas pycnometry, Geological Survey of Denmark and Greenland||||||||||||||||||||||||
OS-95017_H-136|H-136|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|366007|449725|-21.79164|64.52249|76||Basaltgangur um 1 m ţykkur af fín - međalkorna ţóleiíti. |Basalt dike, about 1 m thick of fine-medium-grained tholeiite.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.077|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-137|H-137|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|366343|449404|-21.78436|64.51974|120||Ignimbrít innst í Árdalsgili. Sýni tekiđ viđ hliđina á neđsta fossinum. |Ignimbrite in the innermost part of Árdalsgil. Samples taken next to the bottom waterfall. |Silicic volcanic|Ignimbrite|Smectite-zeolite|2.64|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.121|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-138|H-138|Guđmundsson et al., 1995|Sigurđsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörđur|366353|449400|-21.78415|64.51971|123||Andesít stuđull laus í Árdalsá, óherilega hart ađ taka sýni. Stuđullinn er úr brekkunni ţar fyrir ofan. |Icelandite (andesite) column sample in Ardalsá, very difficult to take a sample. The sample derived from a column in the cliff above. |Intermediate volcanic|Icelandite (andesite)|Smectite-zeolite|2.65|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.004|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Geological Survey of Denmark and Greenland|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-139|H-139|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365916|442135|-21.78656|64.45443|528||Dacít pulsa úr bjargi rétt neđan viđ klettana vestan í Rauđahnjúk. Sýniđ úr vel stuđluđu kubbabergi. |Dacite elongated entablature formation just below the cliffs west of Rauđahnjúkur.|Intermediate volcanic|Dacite|Smectite-zeolite|2.42|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.003|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-140|H-140|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365852|441885|-21.78766|64.45216|476||Líparít, blöđrótt straumflögótt og engin ummyndun greinanleg ţví ţarf ađ láta XRD skera ţar úr. |Vesicular flow-banded rhyolite lava with no alteration apparent, need for XRD.|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.52|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.108|He Gas pycnometry, Geological Survey of Denmark and Greenland|8.88E-18|Measured by Geological Survey of Denmark and Greenland|||2.04E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-141|H-141|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365827|441668|-21.78799|64.45020|453||Basaltandesít, straumflögótt fín - dulkorna og ţétt. Sýni tekiđ úr mosavaxinni skriđu neđan viđ klettabelti sunnan viđ Rauđahnjúk. |Basaltic andesite, flow-banded, fine-grained and dense. Sample taken from mossy skree below a cliff belt to the south of Rauđahnjúkur, |Intermediate volcanic|Icelandite (andesite)|Smectite-zeolite|2.88|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.003|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-142|H-142|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365673|441846|-21.79135|64.45174|463||Móbergsbreksía eđa túff ljósgrćnt til grćnt á lit. Sýni tekiđ úr gili vestan Rauđahnjúks ofan viđ smá stall. |Hyaloclastite breccia or tuff, light-green to green in color. Sample taken from the gorge west of Rauđahnjúkur above a small ledge. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.372|He Gas pycnometry, Geological Survey of Denmark and Greenland|8.07E-16|Measured by Geological Survey of Denmark and Greenland|||1.22E-15|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-143|H-143|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365653|441844|-21.79175|64.45172|464||Gangberg. Sennilega fínkorna smásprunginn keilugangur, grár á lit. Hann liggur nokkuđ óreglulega í gegn um túffiđ og sker einnig líparítganginn. |Intrusion. Probably fine-grained cone sheet, gray in color. Irregular orientation, in the area of a tuff and cuts several rhyolite dykes.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.79|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.008|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|||6.91E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-144|H-144|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365662|441842|-21.79156|64.45170|463||Líparítgangur um 10 m ţykkur. Ummyndađ túff er viđ jađra hans. |Rhyolite dyke about 10 m thick. There is an altered tuff at its edges.|Silicic intrusion|Rhyolite dyke|Smectite-zeolite|2.60|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.158|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-145|H-145|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Skarđsheiđi, to the north of Snók|365661|441837|-21.79159|64.45165|463||Basaltgangur um 0,5 m á ţykkt og er smáblöđróttur. Hann sker líparítganginn. Strik 10° og halli 40° til vesturs. Ath. Sprungufyllingar í túffinu ţarna í kring eru ađallega kalsít.|Basalt dyke about 0.5 m thick and vesicular. It cuts the rhyolite dyke. Strike 10° and dip 40 ° to the west. Note that in the vesicle fillings in the tuff in the area there is an unusual amount of calcite|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.094|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-146|H-146|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Leirá|361835|440996|-21.87020|64.44259|82||Súrt túff, flögótt um 100-200 m utan viđ öskjurima. |Acidic tuff, flaky about 100-200 m outside the caldera rim|Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.293|He Gas pycnometry, Geological Survey of Denmark and Greenland|7.01E-17|Measured by Geological Survey of Denmark and Greenland|||1.18E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-147|H-147|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Leirá|361829|440993|-21.87031|64.44255|81||Súrt túff. Ummyndađ samskonar túff og H-146 međ einhverri súlfíđvirkni Sýnatökustađur ca. 1m frá jarđhitasprungu og ca. 8 m frá gangi (H-148). |Rhyolitic tuff. Altered, same kind of tuff as H-146 with sulfides. Sampling site approx. 1m from geothermal fissure and approx. 8 m from the dyke (H-148)|Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.86|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.198|He Gas pycnometry, Geological Survey of Denmark and Greenland|4.64E-17|Measured by Geological Survey of Denmark and Greenland|||1.68E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-148|H-148|Guđmundsson et al., 1995|Sigurđsson et al., 2000|15.9.1993|Surface|Leirá|361823|440987|-21.87043|64.44250|81||Gangberg. Gangurinn er međalkorna ólivín ţóleiít og sprunginn. Ţykktin 1 m, strik 70°|Intrusion, medium-grained olivine tholeiite with fissures, 1 m thick, striking 70 deg. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.72|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.029|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-149|H-149|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373431|449365|-21.63684|64.52212|106||Basalthraun. Ţunnlögótt fínkorna sprungiđ ţóleiít, ca. 3m ţykkt međ 1 m af karga. Af útfellingum sjást grófur dökkur leir (a.m.k. blandleir), kvars, kalsít og líklega aragónít. |Basaltic lava, thin fine-grained fractured tholeiitic basalt, approx. 3 m thick with 1 m of flow-top breccia. Precipitates show coarse dark clay (mixed clay), quartz, calcite and probably aragonite. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.89|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.025|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|||8.88E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-150|H-150|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373420|449361|-21.63706|64.52207|106||Basalthraun. Nćsta hraunlag ofan viđ H-149, sýni tekiđ úr hlutanum. Lagiđ er um 3 m ţykkt.|Basaltic lava, next lava flow above H-149, sample taken from the section. Layer is about 3 m thick. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.94|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.044|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||9.87E-19|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-151|H-151|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373429|449345|-21.63685|64.52194|107||Basaltkargi. Sýni tekiđ úr kargakenndum toppi sama lags og H-150 og er mjög sprungiđ. Heulandít sést.|Basaltic flow-top breccia. Sample taken from the top of the lava flow H-150 and is very fractured. Heulandite.|Lava flow|Flow-top breccia|Mixed-layer clay|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.103|He Gas pycnometry, Geological Survey of Denmark and Greenland|4.53E-16|Measured by Geological Survey of Denmark and Greenland|||4.83E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-152|H-152|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373441|449330|-21.63661|64.52180|109||Basalthraun. Ţétti hlutinn í nćsta hrauni fyrir ofan H-151, einn fínkorna ţóleiít og um 5 m ţykkt. Helmingurinn er kargakenndur. |Basaltic lava. This part is above H-151, a fine-grained tholeiitic basalt about 5 m thick. Half of it is similar to a flow-top breccia.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.90|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.041|He Gas pycnometry, Geological Survey of Denmark and Greenland|5.92E-18|Measured by Geological Survey of Denmark and Greenland|||1.18E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-153|H-153|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373444|449322|-21.63653|64.52174|110||Basaltkargi. Sama lag og H-152, en nú er sýni tekiđ í miđjum smáblöđróttum kargahlutanum.|Basaltic flow-top scoria. Same layer as H-152, but now the sample is taken from the finely-vesicular flow-top breccia.|Lava flow|Flow-top breccia|Mixed-layer clay|2.91|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.063|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.97E-18|Measured by Geological Survey of Denmark and Greenland|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-154|H-154|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373446|449313|-21.63647|64.52165|110||Basalthraun. Nćsta hraun ofan á 153. Hraunlagiđ er ca. 6 m á ţykkt. |Basaltic lava above H-153, approx 6 m thick.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.89|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.021|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|||7.90E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-155|H-155|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373452|449299|-21.63634|64.52153|111||Basaltkargi. Sýni tekiđ úr karganum ofan á hraunlaginu í H-154. |Basaltic flow-top scoria, taken above sample in H-154.|Lava flow|Flow-top breccia|Mixed-layer clay|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.193|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.81E-17|Measured by Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|2.76E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-156|H-156|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373455|449293|-21.63627|64.52148|112||Basalthraunlag. Nćsta basaltlag ofan á H-155, ţétt fínkorna ţóleiít. Sýni tekiđ um 1 m ofan viđ kargann. Lagiđ er ca 6 m ţykkt međ karga. |Basaltic lava above H-155, compact fine-grained basalt. Sample taken about 1 m above a flow-top breccia. Layer is ca. 6 m thick including the flow-top breccia.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.94|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.012|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-157|H-157|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373468|449279|-21.63599|64.52136|113||Basaltkargi. Úr karganum ofan á H-156. Sýni tekiđ um 20 - 30 m sunnar viđ H-156. |Basaltic lava scoria top above H-156, sample taken approximately 20-30 m to the south of H-156.|Lava flow|Flow-top breccia|Mixed-layer clay|2.84|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.164|He Gas pycnometry, Geological Survey of Denmark and Greenland|1.73E-16|Measured by Geological Survey of Denmark and Greenland|||2.03E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-158|H-158|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373478|449270|-21.63578|64.52128|114||Basalthraun. Nćsta basaltlag ofan viđ H-157. Lagiđ er um 3 m ţykkt.|Basaltic lava above H-157, layer is approximately 3 m thick.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.96|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.047|He Gas pycnometry, Geological Survey of Denmark and Greenland|5.92E-18|Measured by Geological Survey of Denmark and Greenland|||1.28E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-160|H-160|Guđmundsson et al., 1995|Sigurđsson et al., 2000|16.9.1993|Surface|Skarđsheiđi|376061|448665|-21.58152|64.51681|203||Ignimbrít austan í Skarđsheiđi. Steinn í árfarvegi rétt austan viđ skógrćktargirđingar. Ummyndun er óviss.|Ignimbrite east of Skarđsheiđi. A stone in a river channel just east of a forestry fence. Alteration is unclear.|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.073|He Gas pycnometry, Geological Survey of Denmark and Greenland|4.25E-16|Measured by Geological Survey of Denmark and Greenland|||5.40E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-161|H-161|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Dragháls|377828|448285|-21.54442|64.51405|96||Líparít-móberg viđ túff. Móbergsbreksía eđa túff međ dreif af líparíti í. |Rhyolite-hyaloclastite tuff. Hyaloclastite breccia with pieces of rhyolite in it.|Silicic volcanic|Rhyolite tuff|Smectite-zeolite|2.43|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.219|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.65E-14|Measured by Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|3.63E-14|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-163|H-163|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Dragháls|378283|451744|-21.53785|64.54522|272||Líparít úr gili í norđanverđum Skorradal gegnt Draga og austan Vatnsness. Bergiđ er blöđrótt og sýni tekiđ úr lausum stein sem ćttađur er ofar úr hlíđinni sennilega alveg viđ toppinn. |Liparite from a gorge in the northern part of Skorradalur opposite Draga and east of Vatnsness. The rock is vesicular and samples are taken from loose rock that descended from the top of the slope, probably right at the top.|Silicic volcanic|Rhyolite hyaloclastite|Smectite-zeolite|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.088|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-18|Measured by Geological Survey of Denmark and Greenland|||1.88E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-164|H-164|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374612|436117|-21.60091|64.40382|10||Basalthraun. Blöđróttur toppur í hraunlagi. Lámontít er algengt ásamt kalsíti og stilbít etv.|Basaltic lava. Vesicular top of the flow. Laumontite is common as well as calcite and stilbite.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.79|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.090|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-17|Measured by Geological Survey of Denmark and Greenland|||1.22E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-165|H-165|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374623|436118|-21.60069|64.40383|10||Basalthraun, tekiđ úr ţéttari hluta hraunlags H-164, sem er ca. 6m ţykkt. Líklega klórít ummyndun, en pýrít og lámontít sjást. |Basaltic lava taken from the denser part of the lava layer H-164, which is approx. 6 m thick. Probably chlorite altered, but pyrite and laumontite are visible. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.95|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.021|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||6.91E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-166|H-166|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374629|436118|-21.60057|64.40383|10||Basalthraun. Neđri hluti fínkorna ţétts hraunlags etv. blöđrótt um ţađ bil 10 m frá H-165. Í ţví er 20 cm sprunga fyllt af kalsíti međ strik 340° og halli 70° til austurs.|Basaltic lava. The lower part of the fine-grained dense lava flow, somewhat vesicular, approx. 10 m from H-165. Contains 20 cm vein filled with calcite with strike 340° and dip 70° to the east.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.043|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.65E-17|Measured by Geological Survey of Denmark and Greenland|||6.42E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-167|H-167|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374636|436117|-21.60042|64.40383|10||Basalthraun. Tekiđ úr sama basaltlagi og H-166 og er rétt viđ áđurnefnda sprungu. |Basaltic lava, taken from same basalt layer as H-166 and right next to the aforementioned fracture.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.73|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.015|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-168|H-168|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374638|436117|-21.60037|64.40383|10||Basaltgangur. Keilugangur mjög sprunginn og ummyndađur, hallar til ausalćgrar áttar um 15-20°. Ca. 1 m á ţykkt. |Basaltic cone sheets, very fractured and altered. Dips to the east about 15-20 deg. Ca. 1 m thick.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.98|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.109|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-169|H-169|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374644|436120|-21.60025|64.40385|10||Sprungufylling. Tekiđ úr sprungu ţeirri, sem sýni H-167 og H-166 standa viđ, ađ mestu leyti úr kalsíti. |Vein-filling, taken from the fracture that cuts samples H-166 and H-167, mostly appears to be calcite.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.71|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.065|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.36E-17|Measured by Geological Survey of Denmark and Greenland|||5.92E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-170|H-170|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374646|436120|-21.60021|64.40386|11||Basaltgangur, er 30 - 40 cm ţykkur úr ţóleiíti. Strik 140° og halli 10-20° til vesturs. Sýnatökustađur um 4 m vestan viđ H-169. |Basaltic dyke, 30-40 cm thick, tholeiitic. Strike 140° and dip 10-20° to the west. Sampling spot is 4 m west of H-169.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.005|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-171|H-171|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|374671|436121|-21.59970|64.40387|10||Súr gangur eđa rhyolít um ţađ bil 5 m ţykkt. Ca. 100 m vestan hnitapunkts. Varasamt ađ meta strik vegna suglfráviks.|Rhyolitic dyke or rhyolite about 5 m thick. Approx. 100 m west of the coordinate point. Difficult to measure strike due to magnetic effect.|Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.65|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.141|He Gas pycnometry, Geological Survey of Denmark and Greenland|3.06E-17|Measured by Geological Survey of Denmark and Greenland|||5.53E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-172|H-172|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|375055|436082|-21.59171|64.40367|14||Basalthraun. Sýni tekiđ úr ţéttari hluta lagsins, sem er af ţóleiít gerđ. Granat sést vel í berginu, ţ.e. smáir brúnir kristallar, og einnig kvars. |Basaltic lava, sample taken from the dense part of the flow, which is tholeiitic. |Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.96|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.009|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||6.91E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-173|H-173|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|375068|436067|-21.59142|64.40354|14||Líparít innskot, óreglulegt og yngra en basaltgangurinn, um 4 m á breidd. |Rhyolite dyke, irregular and younger than the basalt intrusion, about 4 m wide.|Silicic intrusion|Rhyolite dyke|Epidote-actinolite|2.71|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.100|He Gas pycnometry, Geological Survey of Denmark and Greenland|9.87E-19|Measured by Geological Survey of Denmark and Greenland|||2.96E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-174|H-174|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|375079|436063|-21.76236|64.16189|14||Basaltgangur, fínkorna 50 - 80 cm ţykkur. Stefna 15° og halli 80° til vesturs. |Basaltic dyke, fine-grained, 50-80 cm thick.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.77|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.057|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||4.93E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_H-175|H-175|Guđmundsson et al., 1995|Sigurđsson et al., 2000|17.9.1993|Surface|Hvalfjörđur - Ferstikla, below the farm belonging to Vífil Búason|375087|436059|-21.59102|64.40347|13||Basaltgangur, fínkorna ţóleiít 0,5 m ţykkt, vestan viđ líparítganginn. Virđist eitthvađ ferskari, en ekki sést hvor líparítgangurinn skeri basaltiđ eđur ei.|Basaltic dyke, fine-grained tholeiite 0.5 m thick, west of the rhyolite dyke. Appears somewhat fresh, but not possible to see whether or not the liparite dyke cuts the basalt or the other way around. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.74|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.006|He Gas pycnometry, Geological Survey of Denmark and Greenland|2.96E-18|Measured by Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_HG-1|HG-1|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393077|392359|-21.18684|64.01786|83||Móberg viđ Sauđá, nokkuđ innan viđ bćinn Gufudal, dökkbrúnt međ grćnleitum yrjum, í smektít belti.|Tuff rock by Sauđá, somewhat inside the town of Gufudalur.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.59|Measured on crushed sample by Western Atlas Borehole Laboratories|0.216|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.186|He Gas pycnometry, Western Atlas Borehole Laboratories|5.83E-16|Measured by Geological Survey of Denmark and Greenland|4.54E-16|Measured by Western Atlas Borehole Laboratories|8.68E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-2|HG-2|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393118|392463|-21.18608|64.01880|89||Ţétt ţóleiít hraun, litlu innar, í smektít belti. |Dense tholeiitic basalt, further up in the valley, in smectite alteration zone.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|3.01|Measured on crushed sample by Western Atlas Borehole Laboratories|0.600|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.000|||||||||||||||||||||||||
OS-95017_HG-3|HG-3|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393124|392524|-21.18600|64.01935|93||Ljósgrágrćnt móbergstúff, etv í blandlagi, en innan smektít-beltis, viđ jarđhitasprungu, ca 50 m innan viđ HG-2, viđ ánna. |Light gray-green tuff, perhaps in a mixed layer, but within the smectite zone, by a geothermal fissure, approx. 50 m from HG-2, by the river.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.374|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.371|He Gas pycnometry, Western Atlas Borehole Laboratories|1.32E-16|Measured by Western Atlas Borehole Laboratories|||2.52E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-4|HG-4|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393144|392580|-21.18563|64.01985|95||Ţétt fínkorna ţóleiít hraun nćst fyrir ofna HG-3, ca. 15-20 cm frá jarđhitasprungunni (N40A/75°NV). |Dense fine-grained tholeiitic basalt just above HG-3, approx. 15-20 cm from the geothermal fracture (N40°A/75 °NW).|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.80|Measured on crushed sample by Western Atlas Borehole Laboratories|0.220|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.013|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_HG-5|HG-5|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393205|392668|-21.18445|64.02066|112||Móberg í blandlags-belti nokkru innar. Erfitt var ađ ná nogu löngum kjarna.|Hyaloclastite in a mixed-layer clay zone, some precipitates. Difficult to take long enough Boreholes.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.340|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.297|He Gas pycnometry, Western Atlas Borehole Laboratories|5.36E-16|Measured by Western Atlas Borehole Laboratories|||6.46E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-6|HG-6|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393208|392671|-21.18440|64.02070|113||Laggangur, blöđróttur, holufylltur, 30 cm breiđur.  Viđ HG-5 í blandlags-belti. |Horizontal sill, vesicles filled with precipitates, 30 cm wide. Next to HG-5 in a mixed layer alteration zone.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|2.76|Measured on crushed sample by Western Atlas Borehole Laboratories|0.980|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.087|He Gas pycnometry, Western Atlas Borehole Laboratories|1.38E-17|Measured by Western Atlas Borehole Laboratories|||2.66E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-7|HG-7|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393220|392683|-21.18416|64.02081|116||Svipađur laggangur og HG-6, en 10-15 cm breiđur. |Similar horizontal sill to HG-6, but 10-15 cm wide.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|2.73|Measured on crushed sample by Western Atlas Borehole Laboratories|0.154|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.152|He Gas pycnometry, Western Atlas Borehole Laboratories|9.87E-19|Measured by Western Atlas Borehole Laboratories|||2.96E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-8|HG-8|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393335|392762|-21.18187|64.02155|123||Ennţá ofar međ Sauđá, móberg í blandlags klórít-belti, á sama stađ og Góf og Peter Schiffman tóku sýni H-7 skömmu áđur. |Still higher above Sauđá, tuff in a mixed  clay chlorite belt, in the same place as GÓF and Peter Schiffman took samples H-7.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.232|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.229|He Gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories|||1.48E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-9|HG-9|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393349|392788|-21.18160|64.02178|125||Gangur, sami og sýni H-5 og H-6 í Schiffmans sýnum. |Vein, same as samples H-5 and H-6 in Schiffman's samples.|Hyaloclastite|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.124|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.065|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_HG-10|HG-10|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|93371|392819|-27.27359|63.79955|-1206||Ţétt ţóleít basalt , sama og H-8 (sjá ofar). |Dense tholeiitic basalt, same as H-8 (see above).|Hyaloclastite|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.70|Measured on crushed sample by Western Atlas Borehole Laboratories|0.210|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.017|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_HG-11|HG-11|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393417|392907|-21.18029|64.02287|131||Móbergssýni úr bjargi boriđ niđur ađ Sauđá međ framhlaupi úr Reykjafjalli. |Tuff sample from a rock carried down to Sauđá with a run-off from Reykjafjall.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.366|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.355|He Gas pycnometry, Western Atlas Borehole Laboratories|4.00E-13|Measured by Western Atlas Borehole Laboratories|||5.21E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-12|HG-12|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393426|392918|-21.18011|64.02297|131||Sama og HG-11 en úr fínkornóttara túff. |Same as HG-11 but made of finer grained tuff.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.393|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.373|He Gas pycnometry, Western Atlas Borehole Laboratories|4.55E-13|Measured by Western Atlas Borehole Laboratories|||5.03E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-13|HG-13|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393434|392930|-21.17996|64.02308|132||Áberandi grófkorna, gjallríkt móbergstúff eđa ţursi úr framhlaupsbjargi. Sýni HG-11-13 eru eingöngu palagónítiseruđ en ekki jarđhitaummynduđ.|Prominent coarse-grained, scoria-rich tuff or agglomeritic breccia. Samples HG-13 are only palagonitized but not hydrothermally altered.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.363|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.354|He Gas pycnometry, Western Atlas Borehole Laboratories|1.13E-13|Measured by Western Atlas Borehole Laboratories|||1.41E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-14|HG-14|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393467|392973|-21.17931|64.02348|135||Ţétt ţóleítbasalt úr stuđluđum hluta hrauns, sambćrilegt viđ HG-10 úr bl/kl belti. |Dense tholeiitic basalt from the columnated part of the lava, comparable to HG-10 from bl/kl belt.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|3.00|Measured on crushed sample by Western Atlas Borehole Laboratories|0.600|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.001|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_HG-15|HG-15|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393463|392996|-21.17940|64.02368|140||Basaltgangur (N-S/90, 40 cm) í Grensdalsmyndun viđ Sauđá í kl-belti.  Sama og sýni H-9 og H-10 hjá Schifman. |Basalt dyke (N-S / 90, 40 cm) in Grensdalsmyndun by Sauđá in a chlorite zone. Same as samples H-9 and H-10 at Schifman.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.77|Measured on crushed sample by Western Atlas Borehole Laboratories|0.159|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.154|He Gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories|||7.90E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-16|HG-16|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393469|392995|-21.17928|64.02368|139||Heiđgrćnt móbergstúff 20 cm frá HG-15, sama og H-11 hjá Schifman. |Green tuff 20 cm from HG-15, same as Schifman's H-11.|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.78|Measured on crushed sample by Western Atlas Borehole Laboratories|0.296|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.292|He Gas pycnometry, Western Atlas Borehole Laboratories|1.68E-17|Measured by Western Atlas Borehole Laboratories|||3.75E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_HG-17|HG-17|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393481|393015|-21.17905|64.02386|142||Gangur, 20 cm, stutt frá HG-15. |Intrusion, 20 cm, next to HG-15.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.76|Measured on crushed sample by Western Atlas Borehole Laboratories|0.260|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.002|He Gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_HG-18|HG-18|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Sauđá in the town of Gufudalur in Hveragerđi|393509|393119|-21.17856|64.02480|162||Heiđgrćnt móberg ofar viđ Sauđá ţar sem viđ Schifaman tókum sýni H-12 og HV-1-3, í klórítbelti. |Green tuff above Sauđá, where Schiffman and I took samples H-12 and HV-1-3, in a chlorite belt.|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.83|Measured on crushed sample by Western Atlas Borehole Laboratories|0.320|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.316|He Gas pycnometry, Western Atlas Borehole Laboratories|1.84E-16|Measured by Western Atlas Borehole Laboratories|||2.26E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-1|R-1|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kaldársel í Hjallamisgenginu|360637|394493|-21.85150|64.02539|101||Fínkorna hraun viđ Kaldársel í Hjallamisgenginu.  Sýni R-1 er ca 5 m neđan viđ efri brún helluhraunsins í ţéttasta hluta ţess sem er međ óreglulegar ţverrákir (einskonar stuđlar), en hrauniđ er auk ţess stórstuđlađ ţar sem hver stuđull er um 1 m í ţvermál.|Fine-grained lava at Kaldársel in Hjallamisgengi. Sample R-1 is approx. 5 m below the upper flow margin in the densest part of it with irregular columns of about 1 m in diameter.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.08|Measured on crushed sample by Western Atlas Borehole Laboratories|0.610|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.064|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)|7.36E-16|Measured by Western Atlas Borehole Laboratories|8.88E-17|Measured by Western Atlas Borehole Laboratories|4.38E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-2|R-2|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360626|394479|-21.85170|64.02526|101||Sama hraun og R-1 en 2 m ofar í blöđróttari hluta.|The same lava as R-1 but 2 m higher in the vesicular part.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.08|Measured on crushed sample by Western Atlas Borehole Laboratories|0.135|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.125|He gas pycnometry, Geological Survey of Denmark|1.39E-15|Measured by Western Atlas Borehole Laboratories|1.26E-15|Measured by Western Atlas Borehole Laboratories|1.75E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-3|R-3|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360626|394479|-21.85170|64.02526|101||Sama hraun, ca 2 m ofar.|The same lava, about 2 m higher.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.14|Measured on crushed sample by Western Atlas Borehole Laboratories|0.293|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.286|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)|5.14E-14|Measured by Western Atlas Borehole Laboratories|6.76E-13|Measured by Western Atlas Borehole Laboratories|4.00E-14|Measured by Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-4|R-4|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360640|394483|-21.85142|64.02530|101||Sama hraun, efst.|Same lava, top.|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.97|Measured on crushed sample by Western Atlas Borehole Laboratories|0.414|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.396|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)|7.50E-12|Measured by Western Atlas Borehole Laboratories|3.01E-13|Measured by Western Atlas Borehole Laboratories|7.50E-12|Measured by Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-5|R-5|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360688|394460|-21.85043|64.02511|103||Nćsta hraun ofan viđ R-1 til R-4.  Borađ var niđur í helluhraunsfleka, mjög blöđróttan. |The next lava above R-1 to R-4. It was drilled into a very vesicular lava top.|Lava flow|Flow-top breccia|Unaltered|3.07|Measured on crushed sample by Western Atlas Borehole Laboratories|0.395|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.392|He gas pycnometry, Geological Survey of Denmark|||||1.13E-11|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-6|R-6|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360676|394446|-21.85043|64.02511|103||Nćsta hraun ofan viđ R-1 til R-4.  Borađ var niđur í helluhraunsfleka, mjög blöđróttan. |Same as R-5.|Lava flow|Flow-top breccia|Unaltered|3.03|Measured on crushed sample by Western Atlas Borehole Laboratories|||0.367|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)|8.61E-15|Measured by Western Atlas Borehole Laboratories|1.18E-16|Measured by Western Atlas Borehole Laboratories|8.75E-14|Measured by Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-7|R-7|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360676|394446|-21.85066|64.02498|103||Rauđamalargjall úr bruna í vegi viđ Hjallamisgengiđ. Flokkađ sem kargi í sýnaskrá.|Highly oxidized  glass-rich scoria, from the path to Hjallamisgengur. Categorized as flow-top breccia.|Lava flow|Flow-top breccia|Unaltered|||||0.000|||||||||||||||||||||||||
OS-95017_R-8|R-8|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Reykjanes peninsula, between Valahnúkur and Helgafell|361274|393514|-21.83759|64.01688|137||Jökulbergsset úr móbergi og hálfrúnuđum steinum, milli Valahnúka og Helgafells. |Glacial tillite made of tuff and semi-round stones, between Valahnúkur and Helgafell.|Hyaloclastite|Hyaloclastite sediment|Unaltered|2.62|Measured on crushed sample by Western Atlas Borehole Laboratories|0.285|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.253|He gas pycnometry, Geological Survey of Denmark|2.34E-13|Measured by Western Atlas Borehole Laboratories|||2.51E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-9|R-9|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Valahnúkar|361388|393629|-21.83535|64.01795|146||Ţursamóberg úr Valahnúkum, brúnleitt međ basaltbrotum. |Tuff agglomerate breccia from Valahnúkur, brownish with basalt fragments.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.64|Measured on crushed sample by Western Atlas Borehole Laboratories|0.258|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.236|He gas pycnometry, Geological Survey of Denmark|2.38E-14|Measured by Western Atlas Borehole Laboratories|1.10E-14|Measured by Western Atlas Borehole Laboratories|2.66E-14|Measured by Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-10|R-10|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Helgafell|361367|393347|-21.83553|64.01541|142||Móbergstúff úr Helgafelli, norđaustantil.|Tuff rock from Helgafell, northeast.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.70|Measured on crushed sample by Western Atlas Borehole Laboratories|0.481|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.456|He gas pycnometry, Geological Survey of Denmark|1.77E-12|Measured by Western Atlas Borehole Laboratories|5.86E-13|Measured by Western Atlas Borehole Laboratories|1.87E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-11|R-11|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|East of Helgafell and Valahnúkar|361439|393461|-21.83416|64.01647|145||Hraun austan viđ Helgafell og Valahnúka, tekiđ í misgengisstalli.  Ţetta sýni er ca 3 m neđan yfriborđs, borađ á ská niđur.|Lava east of Helgafell and Valahnúkur, taken from a fault scarp. This sample is about 3 m below the surface, drilled diagonally down.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.08|Measured on crushed sample by Western Atlas Borehole Laboratories|0.141|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.139|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories|9.11E-14|Measured by Western Atlas Borehole Laboratories|9.84E-15|Measured by Western Atlas Borehole Laboratories|1.37E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-12|R-12|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|East of Helgafell and Valahnúkar|361454|393465|-21.83387|64.01650|146||Er úr sama hrauni tekiđ á yfirborđi, lóđrétt niđur í hraunhellu.|From the same lava as R-11, drilled vertically down into the lava.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.07|Measured on crushed sample by Western Atlas Borehole Laboratories|0.313|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.310|He gas pycnometry, Geological Survey of Denmark|6.99E-15|Measured by Western Atlas Borehole Laboratories|||1.14E-14|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-13|R-13|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Helgafell|361128|392916|-21.84001|64.01146|229||Móbergstúff úr austanverđu Helgafelli, fínlagskipt. |Hyaloclastite tuff from the east side of Helgafell, finely layered.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.67|Measured on crushed sample by Western Atlas Borehole Laboratories|0.463|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.456|He gas pycnometry, Geological Survey of Denmark|2.96E-12|Measured by Western Atlas Borehole Laboratories|||2.96E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-14|R-14|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Helgafell|361142|392923|-21.83973|64.01153|225||Sama móbergstúff og R-13 en úr grófkorna lagi, sem virđist gropnara.|The same tuff as R-13 but from a coarse-grained layer, which looks coarser.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.71|Measured on crushed sample by Western Atlas Borehole Laboratories|0.492|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.476|He gas pycnometry, Geological Survey of Denmark|2.09E-12|Measured by Western Atlas Borehole Laboratories|||2.53E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-15|R-15|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|SE of Helgafell|360771|392367|-21.84681|64.00640|229||Móbergstúff, gjallkennt, SA undir Helgafelli.|Hyaloclastite tuff, from a mountainous part, southeast of Helgafell.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.68|Measured on crushed sample by Western Atlas Borehole Laboratories|0.388|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.384|He gas pycnometry, Geological Survey of Denmark|7.18E-13|Measured by Western Atlas Borehole Laboratories|1.53E-13|Measured by Western Atlas Borehole Laboratories|8.01E-13|Measured by Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-16|R-16|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|SW of Helgafell|360072|392553|-21.86126|64.00778|128||Mjög fínkorna móbergstúff SV undir Helgafelli.|Very fine-grained tuff rock SW under Helgafell.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.66|Measured on crushed sample by Western Atlas Borehole Laboratories|0.469|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.453|He gas pycnometry, Geological Survey of Denmark|2.77E-12|Measured by Western Atlas Borehole Laboratories|||2.82E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-17|R-17|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|W of Helgafell|360234|393062|-21.85841|64.01240|130||Mjög gropin hraunhella í hrauninu vestan Helgafells. |Very vesicular lava top west of Helgafell.|Lava flow|Flow-top breccia|Unaltered|3.07|Measured on crushed sample by Western Atlas Borehole Laboratories|0.396|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.394|He gas pycnometry, Geological Survey of Denmark|||4.85E-12|Measured by Western Atlas Borehole Laboratories|3.71E-11|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-18|R-18|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn|353975|385666|-21.97910|63.94355|228||Kleifarvatn, viđ veg norđan til. Ţetta sýni er úr bólstrabroti í ţursabergbreksíu sem er ekki ýkja palagóníseruđ. Af ţeim sökum tókst ekki ađ ná sýni úr túffhlutanum nema úr ţví allra fínkornóttasta sem er sýni R-19|Kleifarvatn, at the road to the north. This sample is from a pillow basalt in breccia that is not overly palagonitized. As a result it was not possible to obtain samples from the tuff section except from the finest grain, which is sample R-19.|Hyaloclastite|Pillow basalt|Unaltered|3.01|Measured on crushed sample by Western Atlas Borehole Laboratories|0.276|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.274|He gas pycnometry, Geological Survey of Denmark|5.70E-13|Measured by Western Atlas Borehole Laboratories|||6.03E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-19|R-19|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn|353978|385664|-21.97905|63.94352|227||Fínkornótt túff, sama stađ og R-18.|Fine-grained tuff, same place as R-18.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.77|Measured on crushed sample by Western Atlas Borehole Laboratories|0.453|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.442|He gas pycnometry, Geological Survey of Denmark|1.03E-14|Measured by Western Atlas Borehole Laboratories|||1.15E-14|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-20|R-20|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352310|382178|-22.00964|63.91159|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|2.96|Measured on crushed sample by Western Atlas Borehole Laboratories|0.236|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.235|He gas pycnometry, Geological Survey of Denmark|1.52E-15|Measured by Western Atlas Borehole Laboratories|||1.56E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-21|R-21|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352309|382184|-22.00966|63.91164|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.255|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.252|He gas pycnometry, Geological Survey of Denmark|2.19E-15|Measured by Western Atlas Borehole Laboratories|||2.94E-15|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-22|R-22|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352308|382190|-22.00968|63.91169|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|3.02|Measured on crushed sample by Western Atlas Borehole Laboratories|0.318|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.317|He gas pycnometry, Geological Survey of Denmark|9.41E-14|Measured by Western Atlas Borehole Laboratories|5.28E-14|Measured by Western Atlas Borehole Laboratories|1.17E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-23|R-23|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352308|382197|-22.00969|63.91176|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|3.04|Measured on crushed sample by Western Atlas Borehole Laboratories|0.330|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.298|He gas pycnometry, Geological Survey of Denmark|2.43E-16|Measured by Western Atlas Borehole Laboratories|||4.04E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-24|R-24|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352310|382206|-22.00967|63.91183|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|3.04|Measured on crushed sample by Western Atlas Borehole Laboratories|0.320|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.297|He gas pycnometry, Geological Survey of Denmark|1.88E-16|Measured by Western Atlas Borehole Laboratories|||2.34E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-25|R-25|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Kleifarvatn úr syđsta tanganum|352312|382214|-22.00964|63.91191|135||Kleifarvatn úr syđsta tanganum (Lambhaga).  Ţar er fallegt ólivín ţóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, ţvermál ca 30-40 cm, óreglulega stuđlađir. Fjögur sýni eru boruđ frá glerkápu inn í bólstrana, en tvö í ţétta innviđi.|Kleifarvatn, from the southernmost peninsula (Lambhaga). There is a beautiful olivine tholeiite pillow basalt on the east side of the beach. Four of these samples are drilled from the glassy cover into the pillow basalt, two into the dense part.|Hyaloclastite|Pillow basalt|Unaltered|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.241|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.240|He gas pycnometry, Geological Survey of Denmark|7.21E-17|Measured by Western Atlas Borehole Laboratories|||9.87E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-26|R-26|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Syđrihöfđi|353108|383759|-21.99492|63.92609|150||Syđrihöfđi.  Fínkornótt túff, borađ hornrétt á lagskiptingu. |Southern part of Kleifarvatn. Fine-grained tuff, drilled perpendicular to the stratification.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|0.470|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.400|He gas pycnometry, Geological Survey of Denmark|1.01E-12|Measured by Western Atlas Borehole Laboratories|||1.05E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-27|R-27|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Syđrihöfđi|353113|383757|-21.99482|63.92608|150||Syđrihöfđi.  Fínkornótt túff, hornrétt á lagskiptingu, í sama túffi og R-26. |Southern part of Kleifarvatn.  Fine-grained tuff, perpendicular to the stratification, in the same tuff as R-26.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.75|Measured on crushed sample by Western Atlas Borehole Laboratories|0.420|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.415|He gas pycnometry, Geological Survey of Denmark|1.39E-12|Measured by Western Atlas Borehole Laboratories|||1.48E-12|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-28|R-28|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Syđrihöfđi|353114|383736|-21.99478|63.92589|150||Syđrihöfđi.  Ţursaberg, borađ í matrixu. |Syđrihöfđi. Agglomerate breccia, drilled into the fine matrix.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|0.283|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.282|He gas pycnometry, Geological Survey of Denmark|1.26E-13|Measured by Western Atlas Borehole Laboratories|||1.41E-13|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_R-29|R-29|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995||Surface|Syđrihöfđi|353104|383733|-21.99498|63.92585|150||Syđrihöfđi.  Bólstrabrot í sama ţursabergi og R-28.|Syđrihöfđi. Pillow basalt in the same breccia as R-28.|Pillow basalt|Pillow basalt|Unaltered|2.98|Measured on crushed sample by Western Atlas Borehole Laboratories|0.197|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.158|He gas pycnometry, Geological Survey of Denmark (1 measurement) and Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories|||1.12E-17|Measured by Geological Survey of Denmark (2 measurements) and Western Atlas Borehole Laboratories (1 measurement)||||||||||||||||||
OS-95017_R-29|R-32|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||Samples R-32 to R-134 are derived from a single outcrop in the Öskuhliđ area in Reykjavik. Samples are taken at different levels within the flow in order to see the variation of petrophysical properties from top to bottom of that flow.The lava is of olivine tholeiite composition dating from the 2nd or 3rd last interglacial. Late Pleistocene coarse-grained olivine basalts of this composition are commonly called grágrýti in Icelandic, in this case the Reykjavik grágrýti. Rocks are assumed to be unaltered, except that some opalline material has precipitated in some of the vugs in the lavas.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.122|He gas pycnometry, Geological Survey of Denmark|2.40E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.76E-15|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-98041_R-33|R-33|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.128|He gas pycnometry, Geological Survey of Denmark|5.15E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||7.81E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.6|||||||||1.61|
OS-98041_R-34|R-34|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.127|He gas pycnometry, Geological Survey of Denmark|4.39E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||7.41E-16|Measured by Geological Survey of Denmark and Greenland||||||||2.4|||||||||1.34|
OS-98041_R-35|R-35|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.129|He gas pycnometry, Geological Survey of Denmark|8.32E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.23E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.3|||||||||1.46|
OS-98041_R-36|R-36|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.126|He gas pycnometry, Geological Survey of Denmark|5.01E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||7.61E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.6|||||||||1.62|
OS-98041_R-37|R-37|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.123|He gas pycnometry, Geological Survey of Denmark|6.20E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||9.33E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.6|||||||||1.38|
OS-98041_R-38|R-38|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.123|He gas pycnometry, Geological Survey of Denmark|1.00E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.47E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.8|||||||||1.56|
OS-98041_R-39|R-39|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.123|He gas pycnometry, Geological Survey of Denmark|||||5.00E-16|||||||||3.3|||||||||1.27|
OS-98041_R-40|R-40|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.131|He gas pycnometry, Geological Survey of Denmark|4.30E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||7.26E-16|Measured by Geological Survey of Denmark and Greenland||||||||2.6|4.1|1.7|||96.0|||||
OS-98041_R-41|R-41|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.113|He gas pycnometry, Geological Survey of Denmark|1.11E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.81E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.5|||||||||0.97|
OS-98041_R-42|R-42|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.128|He gas pycnometry, Geological Survey of Denmark|7.55E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.13E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.7|||||||||1.36|
OS-98041_R-43|R-43|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.123|He gas pycnometry, Geological Survey of Denmark|1.55E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.23E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.4|||||||||1.66|
OS-98041_R-44|R-44|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.124|He gas pycnometry, Geological Survey of Denmark|3.03E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.71E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.5|||||||||1.21|
OS-98041_R-45|R-45|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.130|He gas pycnometry, Geological Survey of Denmark|4.14E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||6.34E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.7|||||||||1.61|
OS-98041_R-46|R-46|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.131|He gas pycnometry, Geological Survey of Denmark|9.17E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.50E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.5|||||||||1.77|
OS-98041_R-47|R-47|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.126|He gas pycnometry, Geological Survey of Denmark|3.32E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.14E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.6|||||||||1.53|
OS-98041_R-52|R-52|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|||||0.000|||||||||||||||||||||||||
OS-98041_R-53|R-53|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|||||0.000|||||||||||||||||||||||||
OS-98041_R-54|R-54|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.327|He gas pycnometry, Geological Survey of Denmark|1.98E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.45E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2|||||||||1.42|
OS-98041_R-55|R-55|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.346|He gas pycnometry, Geological Survey of Denmark|1.52E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.67E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.1|||||||||1.05|
OS-98041_R-56|R-56|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.267|He gas pycnometry, Geological Survey of Denmark|1.27E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.26E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.1|||||||||1.37|
OS-98041_R-57|R-57|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.363|He gas pycnometry, Geological Survey of Denmark|2.25E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.90E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2|||||||||1.08|
OS-98041_R-58|R-58|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.267|He gas pycnometry, Geological Survey of Denmark|1.34E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.37E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.8|||||||||1.28|
OS-98041_R-63|R-63|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.160|He gas pycnometry, Geological Survey of Denmark|2.93E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.03E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.7||||||||||
OS-98041_R-64|R-64|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.141|He gas pycnometry, Geological Survey of Denmark|2.71E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.67E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.6||||||||||
OS-98041_R-65|R-65|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.158|He gas pycnometry, Geological Survey of Denmark|1.95E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.40E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.9|||||||||1.50|
OS-98041_R-66|R-66|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.136|He gas pycnometry, Geological Survey of Denmark|1.76E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.09E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.9|||||||||1.57|
OS-98041_R-67|R-67|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.154|He gas pycnometry, Geological Survey of Denmark|5.41E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||9.05E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.7|||||||||1.63|
OS-98041_R-68|R-68|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.161|He gas pycnometry, Geological Survey of Denmark|1.70E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.98E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2|||||||||1.41|
OS-98041_R-69|R-69|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.166|He gas pycnometry, Geological Survey of Denmark|2.23E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.87E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5|||||||||1.24|
OS-98041_R-70|R-70|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.146|He gas pycnometry, Geological Survey of Denmark|2.88E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.94E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.9|4.2|1.7|||57.0||||1.29|
OS-98041_R-71|R-71|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.176|He gas pycnometry, Geological Survey of Denmark|1.73E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.03E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5|||||||||1.42|
OS-98041_R-72|R-72|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.149|He gas pycnometry, Geological Survey of Denmark|1.66E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.92E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.0||||||||||
OS-98041_R-73|R-73|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.151|He gas pycnometry, Geological Survey of Denmark|1.36E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.41E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3|||||||||1.53|
OS-98041_R-74|R-74|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.153|He gas pycnometry, Geological Survey of Denmark|2.78E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.78E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3|||||||||1.54|
OS-98041_R-76|R-76|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.308|He gas pycnometry, Geological Survey of Denmark|3.46E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.90E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5|||||||||1.06|
OS-98041_R-77|R-77|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.308|He gas pycnometry, Geological Survey of Denmark|1.11E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.98E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.4|||||||||1.33|
OS-98041_R-78|R-78|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.335|He gas pycnometry, Geological Survey of Denmark|1.33E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.35E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.4|||||||||1.29|
OS-98041_R-79|R-79|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.309|He gas pycnometry, Geological Survey of Denmark|3.81E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.86E-15|Measured by Geological Survey of Denmark and Greenland||||||||4.4|||||||||1.32|
OS-98041_R-80|R-80|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.341|He gas pycnometry, Geological Survey of Denmark|1.65E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.90E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.4||||||||||
OS-98041_R-81|R-81|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.326|He gas pycnometry, Geological Survey of Denmark|1.97E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.43E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5||||||||||
OS-98041_R-82|R-82|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.273|He gas pycnometry, Geological Survey of Denmark|1.19E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.11E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5||||||||||
OS-98041_R-83|R-83|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.363|He gas pycnometry, Geological Survey of Denmark|1.33E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.36E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.9|||||||||1.13|
OS-98041_R-85|R-85|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.287|He gas pycnometry, Geological Survey of Denmark|1.76E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.09E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5||||||||||
OS-98041_R-88|R-88|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.297|He gas pycnometry, Geological Survey of Denmark|3.31E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.66E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-98041_R-90|R-90|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.306|He gas pycnometry, Geological Survey of Denmark|2.81E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.83E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3|||||||||1.08|
OS-98041_R-91|R-91|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.264|He gas pycnometry, Geological Survey of Denmark|9.00E-17|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.62E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.7|||||||||1.27|
OS-98041_R-92|R-92|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.314|He gas pycnometry, Geological Survey of Denmark|1.59E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.80E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2||||||||||
OS-98041_R-93|R-93|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.299|He gas pycnometry, Geological Survey of Denmark|2.89E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.95E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3||||||||||
OS-98041_R-94|R-94|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.318|He gas pycnometry, Geological Survey of Denmark|1.91E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.33E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.1|||||||||1.11|
OS-98041_R-95|R-95|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.289|He gas pycnometry, Geological Survey of Denmark|4.77E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||8.02E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2|||||||||1.32|
OS-98041_R-96|R-96|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.293|He gas pycnometry, Geological Survey of Denmark|2.05E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.56E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.5|||||||||1.30|
OS-98041_R-97|R-97|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.312|He gas pycnometry, Geological Survey of Denmark|1.38E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.45E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.0|||||||||1.12|
OS-98041_R-98|R-98|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.333|He gas pycnometry, Geological Survey of Denmark|2.99E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.13E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3||||||||||
OS-98041_R-100|R-100|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.314|He gas pycnometry, Geological Survey of Denmark|1.33E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.36E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2|4.7|2.8|||48.0|||||
OS-98041_R-101|R-101|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.295|He gas pycnometry, Geological Survey of Denmark|3.95E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||6.07E-15|Measured by Geological Survey of Denmark and Greenland||||||||4.3||||||||||
OS-98041_R-102|R-102|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.303|He gas pycnometry, Geological Survey of Denmark|1.33E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.36E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.8|||||||||1.40|
OS-98041_R-103|R-103|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.310|He gas pycnometry, Geological Survey of Denmark|1.60E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.81E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.2||||||||||
OS-98041_R-104|R-104|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.274|He gas pycnometry, Geological Survey of Denmark|1.51E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.66E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.6||||||||||
OS-98041_R-105|R-105|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.305|He gas pycnometry, Geological Survey of Denmark|2.53E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.37E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.9||||||||||
OS-98041_R-106|R-106|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.317|He gas pycnometry, Geological Survey of Denmark|1.69E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.96E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3||||||||||
OS-98041_R-107|R-107|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.08|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.110|He gas pycnometry, Geological Survey of Denmark|7.07E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.06E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.3||||||||||
OS-98041_R-108|R-108|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.08|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.127|He gas pycnometry, Geological Survey of Denmark|1.87E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.96E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.5||||||||||
OS-98041_R-110|R-110|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.129|He gas pycnometry, Geological Survey of Denmark|2.18E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.43E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.4|4.1|1.6|||112.0|||||
OS-98041_R-111|R-111|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.08|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.131|He gas pycnometry, Geological Survey of Denmark|3.63E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||6.18E-16|Measured by Geological Survey of Denmark and Greenland||||||||2.8||||||||||
OS-98041_R-112|R-112|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.110|He gas pycnometry, Geological Survey of Denmark|3.36E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.19E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.7|||||||||1.62|
OS-98041_R-113|R-113|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.120|He gas pycnometry, Geological Survey of Denmark|1.08E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.58E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.3|||||||||1.13|
OS-98041_R-114|R-114|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.113|He gas pycnometry, Geological Survey of Denmark|1.43E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.06E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.3|||||||||1.21|
OS-98041_R-115|R-115|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.111|He gas pycnometry, Geological Survey of Denmark|4.29E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||7.25E-16|Measured by Geological Survey of Denmark and Greenland||||||||2.2|||||||||1.38|
OS-98041_R-116|R-116|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.08|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.113|He gas pycnometry, Geological Survey of Denmark|1.18E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.72E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.3|||||||||1.42|
OS-98041_R-117|R-117|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.117|He gas pycnometry, Geological Survey of Denmark|8.60E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.27E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.8||||||||||
OS-98041_R-118|R-118|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.124|He gas pycnometry, Geological Survey of Denmark|1.04E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.52E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.7||||||||||
OS-98041_R-119|R-119|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.118|He gas pycnometry, Geological Survey of Denmark|9.37E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.38E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.5|||||||||1.59|
OS-98041_R-123|R-123|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.133|He gas pycnometry, Geological Survey of Denmark|2.18E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.09E-14|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-98041_R-124|R-124|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.120|He gas pycnometry, Geological Survey of Denmark|1.14E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.86E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.5||1.7|||65.0||||1.57|
OS-98041_R-125|R-125|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.126|He gas pycnometry, Geological Survey of Denmark|3.71E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||5.71E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.7||||||||||
OS-98041_R-126|R-126|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.115|He gas pycnometry, Geological Survey of Denmark|6.11E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||9.19E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.8|||||||||1.49|
OS-98041_R-127|R-127|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.121|He gas pycnometry, Geological Survey of Denmark|6.36E-15|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||9.55E-15|Measured by Geological Survey of Denmark and Greenland||||||||2.7||||||||||
OS-98041_R-128|R-128|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.116|He gas pycnometry, Geological Survey of Denmark|1.44E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.08E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.5||||||||||
OS-98041_R-129|R-129|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.125|He gas pycnometry, Geological Survey of Denmark|1.04E-14|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.53E-14|Measured by Geological Survey of Denmark and Greenland||||||||2.4||||||||||
OS-98041_R-130|R-130|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.233|He gas pycnometry, Geological Survey of Denmark|1.23E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.18E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.1|||||||||1.27|
OS-98041_R-131|R-131|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.250|He gas pycnometry, Geological Survey of Denmark|1.78E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||3.12E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.8||4.35|2.05||60.0|||||
OS-98041_R-132|R-132|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.244|He gas pycnometry, Geological Survey of Denmark|2.49E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||4.30E-16|Measured by Geological Survey of Denmark and Greenland||||||||3.8|||||||||1.22|
OS-98041_R-133|R-133|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.224|He gas pycnometry, Geological Survey of Denmark|1.00E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||1.80E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.3|||||||||1.97|
OS-98041_R-134|R-134|Friđleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíđ|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|3.05|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Orkustofnun|||0.264|He gas pycnometry, Geological Survey of Denmark|1.16E-16|Measured by Geological Survey of Denmark and Greenland, only reported air apparent permeability; approximate Klinkenberg correction performed by fitting ratio of kg/ki as a function of log10(kg)|||2.06E-16|Measured by Geological Survey of Denmark and Greenland||||||||4.4|||||||||1.17|
OS-95017_S-1|S-1|Guđmundsson et al., 1995|Sigurđsson et al., 2000|20.9.1993|Surface|Lýsuhóll, Snćfellsbćr|299929|489362|-23.22000|64.84465|51||Kjarni úr botni gryfju á útfellingasvćđinu á Lýsuhóli rétt norđan viđ holu 8. |A core from the bottom of a pit in the mineralized area at Lýsuhóll sinter just north of hole 8.|Sediment|Sediment|Smectite-zeolite|2.15|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.477|He gas pycnometry, Geological Survey of Denmark|7.39E-13|Measured by Geological Survey of Denmark and Greenland|2.69E-13|Measured by Geological Survey of Denmark and Greenland|7.57E-13|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-2|S-2|Guđmundsson et al., 1995|Sigurđsson et al., 2000|20.9.1993|Surface|Lýsuhóll, Snćfellsbćr|299935|489362|-23.21987|64.84466|50||Tekiđ á sama stađ nema í toppinum á kísilbreiđunni. |Taken in the same place except at the top of the silica deposit.|Sediment|Sediment|Smectite-zeolite|2.19|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.458|He gas pycnometry, Geological Survey of Denmark|2.58E-13|Measured by Geological Survey of Denmark and Greenland|1.59E-15|Measured by Geological Survey of Denmark and Greenland|4.02E-13|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-3|S-3|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300802|490195|-23.20280|64.85263|222||Granófýr tekinn á hćđ ofan viđ Lýsuhól (H-8). |Granophyre sample taken at a hill above Lýsuhóll (H-8).|Silicic intrusion|Granophyre|Epidote-actinolite|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.068|He gas pycnometry, Geological Survey of Denmark|2.57E-17|Measured by Geological Survey of Denmark and Greenland|||4.64E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-4|S-4|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300803|490389|-23.20305|64.85437|259||Breksía, líklega innskotsbreksía. Ummyndun í epidótbelti og kvars og amfiból sjást í sprungum.|Breccia, probably intrusion-related breccia. Epidote alteration zone. Quartz and amphibole are seen in cracks.|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.005|He gas pycnometry, Geological Survey of Denmark|4.74E-17|Measured by Geological Survey of Denmark and Greenland|||8.29E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-5|S-5|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300803|490414|-23.20309|64.85459|264||Úr granófýr viđ gabbrókontakt. Granófýrinn er grófkorna viđ kontaktinn. Dökka bergiđ viđ kontaktinn virđist vera blanda. E.t.v. Er ţađ blandberg af gabbróinu (glerkennt og dökkt) og ţví súra (ljósara)? Ţađ eru samtíma kvikur.|Granophyre at gabbro contact. The granophore is coarse-grained at the contact. The dark rock at the contact appears to be comagmatic with the granophyre chilling the gabbro but heating the former.|Silicic intrusion|Granophyre|Epidote-actinolite|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.066|He gas pycnometry, Geological Survey of Denmark|4.64E-17|Measured by Geological Survey of Denmark and Greenland|||8.98E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-7|S-7|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300855|490498|-23.20211|64.85538|301||Gabbró ofarlega í gilinu vestan viđ ána, ca. 50 m ofan viđ til austurs, sést í basaltlög sem liggja yfir. |Gabbro high in the gorge west of the river, approx. 50 m above to the east. Basalt lavas can be seen overlying the gabbro.|Basaltic intrusion|Gabbro|Epidote-actinolite|2.90|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.042|He gas pycnometry, Geological Survey of Denmark||||||||||||||||||||||||
OS-95017_S-8|S-8|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300797|490550|-23.20340|64.85581|293||Á sama stađ og S-7. Virđist vera díorítiskt berg, fínkorna og grófkorna. S-8 er grófkorna. |From the same place as S-7. Appears to be a dioritic rock, alternately fine- and coarse-grained. S-8 is coarse-grained.|Intermediate intrusion|Diorite|Epidote-actinolite|2.85|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.060|He gas pycnometry, Geological Survey of Denmark|2.66E-17|Measured by Geological Survey of Denmark and Greenland|||7.40E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-9|S-9|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300797|490550|-23.20340|64.85581|293||Sami steinn og S-8 og tekiđ úr dekkri og fínkornađri hluta steinsins. Fínkornađri hlutinn er eins og innlyksa í grófari hlutanum.|Same rock as S-8 and taken from the darker and finer-grained part of the stone. The fine-grained part is apparently embedded in the coarser part.|Intermediate intrusion|Diorite|Epidote-actinolite|2.90|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.028|He gas pycnometry, Geological Survey of Denmark|1.68E-17|Measured by Geological Survey of Denmark and Greenland|||3.06E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-10|S-10|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300570|489959|-23.20735|64.85038|140||Granófýr eđa rhyolít úr skriđu ofan viđ S-9 upp í hlíđinni vestan í skarđinu. |Granophyre or rhyolite intrusion from a scree above S-9 up the slope west of the pass.|Silicic intrusion|Granophyre|Epidote-actinolite|2.71|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.063|He gas pycnometry, Geological Survey of Denmark|4.24E-17|Measured by Geological Survey of Denmark and Greenland|||9.38E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-11|S-11|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300570|489959|-23.20735|64.85038|140||Granófýr eđa rhyolít úr skriđu ofan viđ S-9 upp í hlíđinni vestan í skarđinu. |Granophyre or rhyolite intrusion from a scree above S-9 up the slope west of the pass.|Silicic intrusion|Granophyre|Epidote-actinolite|2.71|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.051|He gas pycnometry, Geological Survey of Denmark|1.38E-17|Measured by Geological Survey of Denmark and Greenland|||2.66E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-12|S-12|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300570|489959|-23.20735|64.85038|140||Neđarlega í Lýsuskarđi, tekiđ úr 0.5-1 m ţykkum keilugangi, strik 13° halli 30°A.|At the bottom of Lýsuskarđ, Sample taken from a 0.5-1 m thick cone sheet.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.83|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.004|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||2.17E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-13|S-13|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300556|489958|-23.20764|64.85036|136||Hraunlag neđan viđ keiluganginn (S-12), blöđrótt fínkorna líklega 4-6 m thick (basalt?). Ummyndun er klórít-epidót. |Lava flow beneath the cone sheet  (S-12), vesicular, fine-grained, likely 4-6 m thick. Chlorite-epidote alteration zone.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.004|He gas pycnometry, Geological Survey of Denmark|9.87E-18|Measured by Geological Survey of Denmark and Greenland|||1.88E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-14|S-14|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300556|489958|-23.20764|64.85036|136||Tekiđ úr sama lagi og S-13, nema bergiđ virđist blöđróttara, Grasserandi leirfyllt, epidót, kalsedon, kvars o.fl.|Taken from the same layer as S-13, except the rock appears more vesicular. Pores clay-filled, epidote, chalcedony, quartz, etc.|Lava flow|Fine-medium grained basaltic lava|Epidote-actinolite|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.011|He gas pycnometry, Geological Survey of Denmark|2.66E-17|Measured by Geological Survey of Denmark and Greenland|||4.84E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-15|S-15|Guđmundsson et al., 1995|Sigurđsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snćfellsbćr|300494|489806|-23.20874|64.84897|101||Rétt ofan viđ neđsta foss í gilinu. Tekiđ úr keilugangi sem sker granófýrinn í S-16. Bergiđ er fínkorna. Halli 60°, strík 188°.|Just above the lowest waterfall in the gorge. Taken from a cone sheet that cuts the granophyre in S-16. The rock is fine-grained. Dip 60, strike 188.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Epidote-actinolite|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.036|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||2.27E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-17|S-17|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|291475|487904|-23.39561|64.82644|6||Búđarhraun, úr stálinu (ţétta hlutanum). |Postglacial Budarhraun lava flow, from the compact part. |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.09|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.095|He gas pycnometry, Geological Survey of Denmark|8.38E-16|Measured by Geological Survey of Denmark and Greenland|||1.13E-15|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-18|S-18|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|291483|487898|-23.39543|64.82639|6||Búđahraun- úr frauđkennda hlutanum. |Budarhraun lava flow, from the porous part. |Lava flow|Flow-top breccia|Unaltered|3.09|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.170|He gas pycnometry, Geological Survey of Denmark|6.51E-16|Measured by Geological Survey of Denmark and Greenland|3.50E-17|Measured by Geological Survey of Denmark and Greenland|9.62E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-19|S-19|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|278009|483833|-23.67213|64.78136|253||Basaltrík breksía viđ Stapafell viđ veginn. |Basalt breccia at Stapafell by the road.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.72|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.178|He gas pycnometry, Geological Survey of Denmark|8.35E-15|Measured by Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|1.06E-14|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-20|S-20|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|278045|483833|-23.67139|64.78138|257||Sami stađur og S-19. Tekiđ úr bólstrađa basaltinu. |Same place as S-19. Taken from the pillow basalt.|Hyaloclastite|Pillow basalt|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.104|He gas pycnometry, Geological Survey of Denmark|2.37E-17|Measured by Geological Survey of Denmark and Greenland|||3.14E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-21|S-21|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|277808|494474|-23.69296|64.87642|199||Jökulberg (set) Norđan viđ Snćfellsjökul á leiđ niđur. Bergiđ vel samlímt.|Tillite north of Snćfellsjökull on the way down. Rock well cemented. |Sediment|Sediment|Unaltered|2.93|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.178|He gas pycnometry, Geological Survey of Denmark|1.33E-16|Measured by Geological Survey of Denmark and Greenland|||1.77E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-22|S-22|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|277756|494402|-23.69393|64.87574|205||Rauđleitt jökulsbergsset tekiđ rétt ofan viđ virkjun. |Red-colored tillite taken right above the power plant.|Sediment|Sediment|Unaltered|2.89|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.196|He gas pycnometry, Geological Survey of Denmark (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)|4.95E-17|Measured by Geological Survey of Denmark and Greenland (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)|4.93E-18|Measured by Geological Survey of Denmark and Greenland|7.32E-17|Measured by Geological Survey of Denmark (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)||||||||||||||||||
OS-95017_S-23|S-23|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|277792|494472|-23.69328|64.87639|200||Stórstuđlađ bólstra eđa kubbaberg ofan á jökulberginu (S-22). |Columnar pillow or entablature basalt taken above the tillite (S-22).|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.93|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.008|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||1.63E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-24|S-24|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Snćfellsbćr|278593|495350|-23.67780|64.88478|102||Stuđlađ berg líklega eldri grágrýtismyndun skammt ofan viđ Ólafsvík. Gćti veriđ 30 m ţykkt. 20 m af stuđlum og 10 m af kubbabergi. Bergiđ er fínkorna og grátt ađ lit og ólivíndílótt.|Columnar rock probably older Quaternary formation close above Ólafsvík. Could be 30 m thick. 20 m of columns and 10 m of entablature-jointing The rock is fine-grained and gray in color and olivine porphyritic.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.07|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.051|He gas pycnometry, Geological Survey of Denmark|1.68E-17|Measured by Geological Survey of Denmark and Greenland|||2.27E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-25|S-25|Guđmundsson et al., 1995|Sigurđsson et al., 2000|22.9.1993|Surface|Grundarfjarđarbćr|310316|500170|-23.01597|64.94746|21||Kolgrafarfjörđur/Hraunsfjörđur. Grófkorna gabbró, grćnleitt vegna ummyndunnar. Sýni tekiđ viđ veg, ţar sem beygt er inn í Hraunfjörđ. |Kolgrafarfjörđur/Hraunsfjörđur. Coarse-grained basalt, green-colored due to alteration. Sample taken where the road turns into Hraunsfjörđur. |Basaltic intrusion|Gabbro|Chlorite-epidote|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.018|He gas pycnometry, Geological Survey of Denmark|7.70E-17|Measured by Geological Survey of Denmark and Greenland|||1.35E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-26|S-26|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|286613|491258|-23.50280|64.85339|327||Bólstrabergs.- kubbabergsmyndun frá jökulbergsmyndun. Sýniđ er tekiđ úr ţéttum hluta bólstra.|Pillow basalt, entablature formation from sub-glacial  environment. The sample is taken from a dense part of the pillow.|Hyaloclastite|Pillow basalt|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.087|He gas pycnometry, Geological Survey of Denmark|1.48E-17|Measured by Geological Survey of Denmark and Greenland|||2.12E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-27|S-27|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|286613|491258|-23.50280|64.85339|327||Bólstraberg. Sama myndun og S-26 nema sýni tekiđ inn á milli bólstra, mun meira sprungiđ.|Pillow basalt. Same formation as S-26 except the sample was taken in between the pillows, where there are more fractures.|Hyaloclastite|Pillow basalt|Unaltered|3.03|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.073|He gas pycnometry, Geological Survey of Denmark|1.78E-17|Measured by Geological Survey of Denmark and Greenland|||2.02E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-28|S-28|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|286613|491258|-23.50280|64.85339|327||Basalthraun. Líklega úr sömu myndun og S-26 og 27. Stór veruleg stuđlun og vottur af straumflögun.|Basaltic lava, likely from the same formation as S-26 and S-27. Large columns and evidence of flow-banding.|Lava flow|Fine-medium grained basaltic lava|Unaltered|3.03|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.067|He gas pycnometry, Geological Survey of Denmark|2.07E-17|Measured by Geological Survey of Denmark and Greenland|||3.75E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-29|S-29|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|286613|491258|-23.50280|64.85339|327||Móberg. Líklega sama myndun og S-26 - 28. Eins konar móbergshrođi. Sýnatökustađur um 200 m ofan viđ sćluhúsiđ á Fróđárheiđi.|Tuff. Probably the same formation as S-26-28. A kind of tuff. Sampling point about 200 m above the mountain hut at Fróđárheiđi.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.84|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.339|He gas pycnometry, Geological Survey of Denmark|8.57E-13|Measured by Geological Survey of Denmark and Greenland|||8.97E-13|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-30|S-30|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|283383|493117|-23.57355|64.86794|261||Lagskipt túff. Ath. sýni 30-33 öll úr sömu myndun, sýnin tekin innan 10 m2. Bergiđ virđist vera ólivín-plagíóklasdílótt. |Layered tuff. Samples 30-33 all from the same formation, samples taken within 10 m of each other. The rock appears to be olivine-plagioclase porphyritic.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.86|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.267|He gas pycnometry, Geological Survey of Denmark|2.64E-14|Measured by Geological Survey of Denmark and Greenland|4.42E-15|Measured by Geological Survey of Denmark and Greenland|2.48E-14|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-31|S-31|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|283383|493117|-23.57355|64.86794|261||Blóđrauđur móbergshrođi.|Highly oxidized and highly porous tuff.|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.00|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.271|He gas pycnometry, Geological Survey of Denmark||||||||||||||||||||||||
OS-95017_S-32|S-32|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|283383|493117|-23.57355|64.86794|261||Basalthraun. Sýni tekiđ úr vel kristölluđum stuđli um 30 cm breiđum.|Basaltic lava. Sample taken from well-crystallized and 30 cm wide entablature. |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.06|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.056|He gas pycnometry, Geological Survey of Denmark|3.06E-17|Measured by Geological Survey of Denmark and Greenland|||4.74E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-33|S-33|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Fróđárheiđi, Snćfellsness|283383|493117|-23.57355|64.86794|261||Bólstraberg. Sýni tekiđ úr ca. 10 cm stuđli.|Pillow lava. Sample taken from  a 10 cm wide entablature.|Hyaloclastite|Pillow basalt|Unaltered|3.04|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.072|He gas pycnometry, Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (4 measurements)|5.43E-18|Measured by Geological Survey of Denmark and Greenland (2 measurements) and Western Atlas Borehole Laboratories (2 measurements)|||1.09E-17|Measured by Geological Survey of Denmark (3 measurements) and Western Atlas Borehole Laboratories (2 measurements)||||||||||||||||||
OS-95017_S-34|S-34|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Búlandshöfđi, Grundarfjörđur|287906|501466|-23.49087|64.94554|92||Basalthraun. Međal-grófkorna ólivín-ţóleiítbasalt e.t.v. Í tertíera hluta Búlandshöfđa, áberandi kúluveđrun. Sýni tekiđ viđ veginn í ca. 60 m hćđ. |Basalt lava. Medium-coarse-grained olivine-tholeiite basalt. Perhaps in the tertiary part of Búlandshöfđi, noticeable erosion. Samples taken by the road at approx. 60 m elevation.|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.96|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.071|He gas pycnometry, Geological Survey of Denmark|1.85E-16|Measured by Geological Survey of Denmark and Greenland|||2.86E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-35|S-35|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Grundarfjarđarbćr|304343|499577|-23.14125|64.93870|7||Basalthraun. Tertíert fínkorna ţóleiíthraun međ kalsedón og jaspis í sprungum.|Basaltic lava. Tertiary fine-grained tholeiitic lava with chalcedony and jasper in veins. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.92|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.013|He gas pycnometry, Geological Survey of Denmark|8.88E-18|Measured by Geological Survey of Denmark and Greenland|||1.78E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-36|S-36|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|304232|499812|-23.14393|64.94074|1||Andesít. Fín - dulkorna andesítgangur. Sýni tekiđ í Eiđisstapa, ţann er Landstapi heitir, sunnan viđ Sjóstapa.|Fine-grained, andesite dyke. Samples taken in Eiđisstapi, the one called Landstapi, south of Sjóstapi.|Intermediate intrusion|Diorite|Chlorite-epidote|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.007|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||2.27E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-37|S-37|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|303754|497146|-23.15031|64.91659|199||Hraunlag. Međalkorna ólivín-ţóleiítbasalt, líklega um 8 m ţykkt. Sýni tekiđ úr gili ofan viđ ćfingasvćđi Skotfélagsins. |Lava flow, medium-grained olivine tholeiite, likely 8 m thick. Sample taken from the gorge above the practice area for the Rifle association. |Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.88|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.011|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||2.37E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-38|S-38|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|303789|497141|-23.14956|64.91657|188||Súrt innskot. Sýni tekiđ úr stuđlupu blöđróttu bergi. Stuđlar um 25 cm breiđir. Pýrít sést í berginu.|Acidic intrusion. Sample taken from a columnar vesicular rock, approx. 25 cm broad. Pyrite is visible.|Silicic intrusion|Rhyolite dyke|Chlorite-epidote|2.66|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.124|He gas pycnometry, Geological Survey of Denmark|2.17E-16|Measured by Geological Survey of Denmark and Greenland|||3.76E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-39|S-39|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|303809|497141|-23.14915|64.91658|183||Súrt berg. Sýni tekiđ úr eins konar blandbergi og var ţetta úr súra hlutanum.|Acidic rock. Sample taken from some kind of comagmatic mixed rock. Sample belonging to the acidic part. |Silicic intrusion|Rhyolite dyke|Chlorite-epidote|2.66|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.006|He gas pycnometry, Geological Survey of Denmark|1.78E-17|Measured by Geological Survey of Denmark and Greenland|||3.26E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-40|S-40|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|303809|497141|-23.14915|64.91658|183||Basalt. Sama berg og S-39 og nú tekiđ úr basalthlutanum. |Basalt intrusion, same rock as S-39 but now taken from the basaltic part. Co-magmatic with the rhyolite part |Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.014|He gas pycnometry, Geological Survey of Denmark|8.88E-18|Measured by Geological Survey of Denmark and Greenland|||1.78E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-41|S-41|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|305545|495987|-23.11095|64.90727|198||Basalthraun. Grófkorna ólivín-ţóleiítbasalt. Ofarlega í ţví er 0,5 - 1 m ţykkur keilugangur, sem liggur undir Setberg I. |Basalt lava. Coarse-grained olivine-tholeiite basalt. At the top of it is a 0.5-1 m thick cone sheet, which lies under Setberg I.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.95|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.050|He gas pycnometry, Geological Survey of Denmark|2.07E-17|Measured by Geological Survey of Denmark and Greenland|||3.85E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-42|S-42|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|306578|500532|-23.09539|64.94856|20||Ísúrt berg. Ísúr keilugangur í gabbrói viđ vegkannt. |Intermediate rock. Intermediate cone sheet in gabbro by the roadside.|Intermediate intrusion|Diorite|Chlorite-epidote|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.004|He gas pycnometry, Geological Survey of Denmark|7.90E-18|Measured by Geological Survey of Denmark and Greenland|||1.58E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-43|S-43|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|306882|501300|-23.09003|64.95560|18||Gabbró. Sýni tekiđ viđ vegkannt, grófkorna og grćnleitt á lit. |Gabbro, sample taken by the roadside, coarse-grained and greenish in color.|Basaltic intrusion|Gabbro|Chlorite-epidote|2.88|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.007|He gas pycnometry, Geological Survey of Denmark|7.90E-18|Measured by Geological Survey of Denmark and Greenland|||1.58E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-44|S-44|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|306988|501339|-23.08785|64.95601|20||Gabbró. Sýni tekiđ viđ vegkannt um 20 m NA viđ S-43. Steinarnir eru ćttađir úr klettum beint fyrir ofan sýnatökustađina. |Gabbro, sample taken by the roadside approx. 20 m northeast of S-43. The rocks are descended from cliffs directly above the sampling points.|Basaltic intrusion|Gabbro|Chlorite-epidote|3.10|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.017|He gas pycnometry, Geological Survey of Denmark|4.91E-16|Measured by Geological Survey of Denmark and Greenland|||6.66E-16|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-45|S-45|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|306974|501367|-23.08818|64.95626|15||Gabbró, tekiđ á sama stađ og S-44. |Gabbro, taken from the same place as S-44. |Basaltic intrusion|Gabbro|Chlorite-epidote|2.91|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.010|He gas pycnometry, Geological Survey of Denmark|1.28E-17|Measured by Geological Survey of Denmark and Greenland|||2.37E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-46|S-46|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|306974|501367|-23.08818|64.95626|15||Gabbró, tekiđ á sama stađ og S-44.|Gabbro, taken from the same place as S-44. |Basaltic intrusion|Gabbro|Chlorite-epidote|3.21|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.011|He gas pycnometry, Geological Survey of Denmark|1.38E-17|Measured by Geological Survey of Denmark and Greenland|||2.47E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_S-47|S-47|Guđmundsson et al., 1995|Sigurđsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörđur|307007|501460|-23.08760|64.95711|9||Gabbró, mjög grófkorna og er ca. 100 m austan viđ S-46 viđ veginn. Um 3 cm langir pýroxen stönglar áberandi. |Gabbro, very coarse-grained and approx. 100 m east of S-46 by the road. Approx. 3 cm long pyroxene visible. |Basaltic intrusion|Gabbro|Chlorite-epidote|2.98|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.011|He gas pycnometry, Geological Survey of Denmark|1.18E-17|Measured by Geological Survey of Denmark and Greenland|||2.27E-17|Measured by Geological Survey of Denmark and Greenland||||||||||||||||||
OS-95017_E-13|E-13|Guđmundsson et al., 1995|Sigurđsson et al., 2000|27.8.1993|Surface|Reykjavik|363325|421973|-21.82166|64.27272|94||Gangberg. 2 m ţykkur međalkorna ţóleiítgangur. Sýni tekiđ u.ţ.b. úr miđjum ganginum, sem er í gilinu ofan viđ fossinn. |Intrusion, 2 m thick medium-grained tholeiitic intrusion. Sample taken from the middle of the dyke, from the gorge above the waterfall.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Smectite-zeolite|2.94|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.068|He gas pycnometry, Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)|1.41E-17|Measured by Western Atlas Borehole Laboratories (1 measurement) and Geological Survey of Denmark (2 measurements)|||2.96E-17|Measured by Western Atlas Borehole Laboratories (1 measurement) and Geological Survey of Denmark (2 measurements)||||||||||||||||||
OS-95017_E-28|E-28|Guđmundsson et al., 1995|Sigurđsson et al., 2000|6.9.1993|Surface|Mosfellsbćr|376333|414227|-21.54697|64.20826|153||Dólerít? veđrunarútlínur eins og í ólivínţóleiíti, bergiđ virtist gjallkennt og blöđrótt. Lagiđ liggur í hlíđinni miđri eđa rétt ofan viđ skriđu. |Dolerite, looks like olivine tholeiite, vesicular. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.96|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.108|He gas pycnometry, Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)|4.56E-16|Measured by Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)|1.58E-17|Measured by Geological Survey of Denmark and Greenland|5.55E-16|Measured by Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)||||||||||||||||||
OS-95017_E-31|E-31|Guđmundsson et al., 1995|Sigurđsson et al., 2000|6.9.1993|Surface|Mosfellsbćr|376346|414234|-21.54672|64.20832|153||Fínkorna innskot (silla) um ţađ bil 4 m ofan viđ E-30 (Dólerítiđ? E-28)|Fine-grained intrusion (sill) approximately 4 m above E-30 (Dolerite? E-28)|Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|||||0.000|||||||||||||||||||||||||
OS-95017_EŢ-3|EŢ-3|Guđmundsson et al., 1995|Sigurđsson et al., 2000|26.8.1993|Surface|Reykjavik|366676|414856|-21.74618|64.21026|54||Dólerít innskot. Í stórum steini um 2 m frá EŢ-1 og EŢ-2. |Doleritic intrusion.|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||0.003|He gas pycnometry, Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)||||||||||||||||||||||||
OS-95017_KH-3|KH-3|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|42|Dýpi 42.43-42.63 m, basalt breksía.|Basalt breccia. |Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.85|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.269|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.253|He gas pycnometry, Western Atlas Borehole Laboratories|1.01E-16|Measured by Western Atlas Borehole Laboratories|||1.72E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-4|KH-4|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|45|Dýpi 44.95-45.10 m, Halarauđur.|Halarauđur (special ignimbrite layer). |Silicic volcanic|Ignimbrite|Smectite-zeolite|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.125|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.124|He gas pycnometry, Western Atlas Borehole Laboratories|2.96E-18|Measured by Western Atlas Borehole Laboratories|||6.91E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-5|KH-5|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|47|Dýpi 46.75-46.9 m, Halarauđur úr kassa 4 (rauđ og svört sambreiskja).|Halarauđur from box 4 (red and black breccia).|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.165|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.164|He gas pycnometry, Western Atlas Borehole Laboratories|4.93E-18|Measured by Western Atlas Borehole Laboratories|||1.18E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-6|KH-6|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|49|Dýpi 48.95-49.10, Halarauđur - gráleitur međ rauđum molum í en ekki sambrćdd eđa međ slíkum strúktúr heldur eins og breksían sé samlímd og hafi ekki runniđ til.|Halarauđur - greyish with red crumbs but not fused or with such a structure but as if the breccia filter is cemented and has not slipped.|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.71|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.216|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.213|He gas pycnometry, Western Atlas Borehole Laboratories|4.84E-17|Measured by Western Atlas Borehole Laboratories|||9.18E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-7|KH-7|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|54|Dýpi 54.13-54.23. Neđan viđ Halarauđ. Grásvört samlímd (líklega međ zeólítum) breksía.|Below Halarauđur. Grey-black cemented, likely with zeolites, breccia.|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.157|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.157|He gas pycnometry, Western Atlas Borehole Laboratories|1.79E-16|Measured by Western Atlas Borehole Laboratories|||2.16E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-8|KH-8|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|59|Dýpi 59.1-59.25 m, grábrún breksía (ath. lýsingu úr kassa 6).|Grey-brown breccia (attention description originally box 4)|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.160|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.160|He gas pycnometry, Western Atlas Borehole Laboratories|1.09E-17|Measured by Western Atlas Borehole Laboratories|||2.37E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-9|KH-9|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|64|Dýpi 63.9-64.0 m, blöđrótt grátt basalt og ţađ sést glitta á pýrít.|Vesicular grey basalt with visible pyrite. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.95|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.173|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.172|He gas pycnometry, Western Atlas Borehole Laboratories|7.01E-17|Measured by Western Atlas Borehole Laboratories|||1.24E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-10|KH-10|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|69|Dýpi 68.5-68.6 m, fínkornótt smásprungiđ basalt og hálf blöđrufyllt.|Fine-grained, finely-fractured basalt with vesicles half-filled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.84|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.217|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.216|He gas pycnometry, Western Atlas Borehole Laboratories|5.92E-18|Measured by Western Atlas Borehole Laboratories|||1.38E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-11|KH-11|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|77|Dýpi 76.8-76.9 m, Útfellingaríkt móbergstúff.|Amygdale-rich hyaloclastite tuff.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.327|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.319|He gas pycnometry, Western Atlas Borehole Laboratories||||||||||||||||||||||||
OS-95017_KH-12|KH-12|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|87|Dýpi 87.1-87.2 m, fínkornótt basalt.|Fine-grained basalt. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.85|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.132|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.121|He gas pycnometry, Western Atlas Borehole Laboratories|1.53E-17|Measured by Western Atlas Borehole Laboratories|||2.81E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-13|KH-13|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|94|Dýpi 94.3-94.4 m, Basaltbreksía milli hraunlaga og er ljósgrćn á lit.|Basalt breccia between lava flows and light green in color.|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.67|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.113|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.113|He gas pycnometry, Western Atlas Borehole Laboratories|4.93E-18|Measured by Western Atlas Borehole Laboratories|||1.09E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-14|KH-14|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|115|Dýpi 115.2-115.3 m, sćmilega - illa kristallađ fín-međalkorna ljósgrátt basalt.|Medium-poorly crystallized fine-medium grained light green basalt.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.184|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.176|He gas pycnometry, Western Atlas Borehole Laboratories|6.61E-17|Measured by Western Atlas Borehole Laboratories|||9.67E-17|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-15|KH-15|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|127|Dýpi 127.33-127.43 m, fínkornótt blöđrótt basalt.|Fine-grained vesicular basalt. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.118|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.117|He gas pycnometry, Western Atlas Borehole Laboratories|6.91E-18|Measured by Western Atlas Borehole Laboratories|||9.87E-18|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-95017_KH-16|KH-16|Sigurđsson and Stefánsson, 1994|Guđmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarđ hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|131|Dýpi 131.2 - 131.3, samţjappađ móberg eđa túff.|Compacted hyaloclastite or tuff. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.68|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.190|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.184|He gas pycnometry, Western Atlas Borehole Laboratories|7.01E-17|Measured by Western Atlas Borehole Laboratories|||1.33E-16|Measured by Western Atlas Borehole Laboratories||||||||||||||||||
OS-99024_ÖJ-1-1|ÖJ-1-1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|795|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote||||||||||||||||||||||||||||||
OS-99024_ÖJ-1-2|ÖJ-1-2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|795|Međalögrófkorna mjög ummyndađ og eđa blöđrótt basalt|Medium-grained highly altered and/or vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote||||||||||||||||||||||||||||||
OS-99024_ÖJ-1-5|ÖJ-1-5|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote||||||||||||||||||||||||||||||
OS-99024_ÖJ-1-6.1|ÖJ-1-6.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|||||||||||404|0.0024740|||||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-6.2|ÖJ-1-6.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.149|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.146|He gas pycnometry, Geological Survey of Denmark and Greenland|1.68E-17|Measured by Geological Survey of Denmark and Greenland|7.90E-18|Measured by Geological Survey of Denmark and Greenland|3.75E-17|Measured by Geological Survey of Denmark and Greenland|348|0.0028711||0.000229687|12.5||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-7|ÖJ-1-7|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|||||0.000|||||||||||||||||||||||||
OS-99024_ÖJ-1-7.1|ÖJ-1-7.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.77|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.148|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.149|He gas pycnometry, Geological Survey of Denmark and Greenland|2.86E-17|Measured by Geological Survey of Denmark and Greenland|3.95E-18|Measured by Geological Survey of Denmark and Greenland|4.15E-17|Measured by Geological Survey of Denmark and Greenland|247|0.0040486||0.000456951|8.86||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"||3.49||2.06|0.3||26.0|10.6||2.77|
OS-99024_ÖJ-1-7.2|ÖJ-1-7.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.83|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.143|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.136|He gas pycnometry, Geological Survey of Denmark and Greenland|||5.92E-18|Measured by Geological Survey of Denmark and Greenland|||177|0.0056433||0.000884536|6.38||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-8.2|ÖJ-1-8.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.165|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.150|He gas pycnometry, Geological Survey of Denmark and Greenland|1.88E-17|Measured by Geological Survey of Denmark and Greenland|5.92E-18|Measured by Geological Survey of Denmark and Greenland|4.15E-17|Measured by Geological Survey of Denmark and Greenland|193|0.0051813||0.000747669|6.93||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-9.1|ÖJ-1-9.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.164|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.161|He gas pycnometry, Geological Survey of Denmark and Greenland|2.66E-17|Measured by Geological Survey of Denmark and Greenland|6.91E-18|Measured by Geological Survey of Denmark and Greenland|5.43E-17|Measured by Geological Survey of Denmark and Greenland|163|0.0061425||0.001051799|5.84||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"||3.62||2.12|0.3||27.6|11.2||2.52|
OS-99024_ÖJ-1-10.1|ÖJ-1-10.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.163|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.155|He gas pycnometry, Geological Survey of Denmark and Greenland|5.43E-17|Measured by Geological Survey of Denmark and Greenland|1.38E-17|Measured by Geological Survey of Denmark and Greenland|7.60E-17|Measured by Geological Survey of Denmark and Greenland|171|0.0058343||0.000948668|6.15||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-10.2|ÖJ-1-10.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.176|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.175|He gas pycnometry, Geological Survey of Denmark and Greenland|4.93E-17|Measured by Geological Survey of Denmark and Greenland|1.28E-17|Measured by Geological Survey of Denmark and Greenland|8.98E-17|Measured by Geological Survey of Denmark and Greenland|113|0.0088731||0.002196315|4.04||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-11.1|ÖJ-1-11.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.189|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.185|He gas pycnometry, Geological Survey of Denmark and Greenland|1.03E-16|Measured by Geological Survey of Denmark and Greenland|3.65E-17|Measured by Geological Survey of Denmark and Greenland|1.41E-16|Measured by Geological Survey of Denmark and Greenland|162|0.0061690||0.001061795|5.81||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
OS-99024_ÖJ-1-11.2|ÖJ-1-11.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|798|Hlutkristallađ móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.81|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume); measured by Geological Survey of Denmark and Greenland|0.244|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.197|He gas pycnometry, Geological Survey of Denmark and Greenland|1.41E-16|Measured by Geological Survey of Denmark and Greenland|1.21E-16|Measured by Geological Survey of Denmark and Greenland|2.89E-16|Measured by Geological Survey of Denmark and Greenland|158|0.0063131||0.001111467|5.68||"Room temperature measurements by Geological Survey of Denmark and Greenland; Formation resistivity factor is ""apparent"", i.e. resistivity of sample / resistivity of brine. Resistivity measured as impedance to AC signal of 1 KHz frequency"|||||||||||
ÍSOR-2011/064_150803-01|150803-01|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|West of Hveradalaskálinn|382146|393411|-21.41103|64.04242|259||Lagskipt túff. Kjarnar samsíđa laskiptingu. Lagskipting óregluleg vegna hreyfingar innan túffsins á gostíma.|Layered tuff. Boreholes parallel to layering. Layering irregular due to postsedimentation movement during eruption|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.52|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.431|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|5.38E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.65E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.5|2.34||||15.0|||||
ÍSOR-2011/064_150803-03|150803-03|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|West of Hveradalaskálinn|382147|393392|-21.41099|64.04225|259||Fínkorna túff. Kjarni samsíđa lagskiptingu|Fine grained layer. Borehole parallel to layering.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.376|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.45E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.51E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.0|||||14.0|||||
ÍSOR-2011/064_150803-04|150803-04|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|West of Hveradalaskálinn|382158|393411|-21.41078|64.04243|259||Grófkorna túss. (korn <1cm). Strikstefna lagsins er 354°og halli 6°V.  Mikill halli vegna snúnings lags eftir gos. |Coarse grained tuff (grains <1 cm). Strike of layer 354°dip 6°W. Steep dip due to postdepositional rotation. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.64|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.426|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.82E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.92E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.5|1.90||||12.9|||||
ÍSOR-2011/064_150803-05|150803-05|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|Votuklettar-Threngsli|380188|387680|-21.44651|63.99035|333||"Skriđukennt ""foreset"" lagskipting, halli 25° og strikstefna 351°. Kornastćrđ <1cm "|Avalanche type of foreset bedding, dip 25°,strike 351°. Grain size <1 cm |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.157|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.50E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.85E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.3|4.30||||79.0|||||
ÍSOR-2011/064_150803-06|150803-06|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|Votuklettar-Threngsli|380188|387680|-21.44651|63.99035|333||Lárétt lagskipt túff. Kornastćrđ <0,5cm. Kjarni ţvert á lagskiptingu|From horizontally layered tuff, grain size <0.5 cm. Drilling perpendicular to layering. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.28|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.298|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|5.65E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||6.46E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.3||||||||||
ÍSOR-2011/064_150803-08|150803-08|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|Votuklettar-Threngsli|379834|387951|-21.45394|63.99265|277||Fínkorna tuff, strikstefna 1°, halli 2°E. Lagskipting ca. 1cm ţykk lög. Kjarni ţvert á lagskiptingu|Fine grained tuff. Strike 1°, dip 2°E. layering ~1 cm thick. Drilling parallel to layering. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.58|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.343|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.05E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.61E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.5|2.85||||37.0|||||
ÍSOR-2011/064_150803-10|150803-10|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|Slightly west of Votuklettar|379835|388040|-21.45399|63.99345|272||Túffríur blettur innan  breksíu innan gígs. Litaskipti  í kjarnanum frá yfirborđi inn í neđri hluta kjarnans. Unur í palagonitiseringu innan og utan gígsins. |Tuff-rich patch within primary breccia within crater. Colour change from surface to inner part of Borehole. Note palagonite difference outside and inside crater. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.303|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.16E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.74E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.0|2.65||||43.0|||||
ÍSOR-2011/064_170803-01|170803-01|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Stora Dímon|405170|414657|-20.95377|64.23387|390||Suđurhlíđar Stóra Dímons. Líklegast jökulberg, Korn ávöl.|South slope of Stóra Dímon. Probably till. Rounding observed in pebbles|Sediment|Sediment|Unaltered|2.52|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.379|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.05E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.10E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||0.9|1.15||||2.2|||||
ÍSOR-2011/064_170803-02|170803-02|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|West side of Stóra dímon|405295|414873|-20.95133|64.23584|406||Prímert túff. Titölulega grófkorna (<1cm), gróf lagskipting. |Primary tuff. Relatively coarse grained (<1 cm), coarse layering.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.64|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.403|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.22E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.21E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.1|1.50||||1.8|||||
ÍSOR-2011/064_170803-03|170803-03|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll eldri- south exposure|410385|421770|-20.85068|64.28650|539||Opna til suđurs, tuff lagst til ofan vatnsborđs og nćrri gígnum. Efsti hluti kjarnans oxiderađur, sem hverfur um 2-3 cm neđar. |South exposure. sub-aerial and near crater. Top of Boreholes with reddish oxidation, which disappears after 2-3 cm from surface. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.68|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.533|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.66E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.78E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|||||3.1|||||
ÍSOR-2011/064_170803-04|170803-04|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll eldri- south exposure|410437|421747|-20.84959|64.28630|542||Túff millimassi milli stćrri túffmola (t.d. Sýni 3). Prímert túff međ engri sjáanlegri lagskiptingu.|Tuff media into which the large tuff fragments (e.g. sample 3) are embedded. Primary and no bedding visible.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.54|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.423|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.01E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.09E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.1|1.70||||2.8|||||
ÍSOR-2011/064_170803-05|170803-05|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll eldri- south exposure|410437|421747|-20.84959|64.28630|542||"Túff hlunkur innan ""yngra túffs"". Gróf lagskipting. Sýni tekiđ um 5 m frá sýni 4. Oxun vart sjáanleg. "|"Tuff boulder embedded in ""younger"" tuff. Coarse layering. Sample taken about .5 m away from sample 4. Oxidation near absent. "|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.498|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.20E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.19E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.1|1.65||||4.8|||||
ÍSOR-2011/064_170803-06|170803-06|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll eldri- north exposure|411861|422596|-20.82070|64.29429|550||"Túff neđan Yngri Skefilsfjallsmyndun, um 5 m frá bólstrabergs ""innskoti"". Lagskiptingin hallar um 6-7°. Eitthvađ uppbrot í túffinu. Túffiđ er dökkbrúnt efst en verđur dekkra er neđar kemur í kjarnanum. Sýni tekiđ í rofnum hluta túffsins. "|Tuff below the younger Skefislfjöll. about .5 m from a pillow basalt intrusion. Layering dips about 6-7°. Some breakup apparent in tuff, dark brown in top part of Borehole but becomes darker in lower part of Borehole. Sample taken in an erosional gully. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.439|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|5.44E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.56E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.10||||9.3|||||
ÍSOR-2011/064_170803-07|170803-07|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll yngri (last glaciation)|412642|423562|-20.80515|64.30315|543||Túff, ađeins grófara en sýni 38, (kornastćrđ 5-1 cm. Yfirborđsoxun hverfandi. Lagskiptin 1-3 m ţykk. Kjarni tekin samsíđa lagskiptingu. |Tuff, a little coarser than sample 38, (grain size < ,5 cm) Surface oxidation negligible. Layering 1-3 m thick. Borehole parallel to layering|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.424|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|6.38E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||6.50E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.00||||5.1|||||
ÍSOR-2011/064_170803-08|170803-08|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll yngri (last glaciation)|412636|423548|-20.80526|64.30302|541||Fín lagskipt túff, laskipting 5-1 cm. Sýni 8 er um 2-3 m hćrra upp en sýni 17837. setzt til í vatni og rofeinkenni augljós í túffinu. Túffiđ mjög fínkorna (<1mm)|Fine layered tuff. Layering ,5-1 cm. Sample 8 is about 2-3 m higher up than 17837. Water action clear and erosional features observed in tuff. Tuff very fine grained (<1 mm) |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.67|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.399|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.66E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.73E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.9|1.90||||13.0|||||
ÍSOR-2011/064_170803-09|170803-09|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Skefilsfjoll yngri (last glaciation)|412877|424065|-20.80059|64.30772|560||Prímert túff brekksía. Laghalli um 8°.  Túff straumurinn líklega viđ lóđréttan jađar jökulís. Misleitni líklega á milli einstakra kjarna. |Primary tuff breccia. Layer inclination about 8°W. Tuff probably avalanching down beside vertical glacier. Heterogenity expected between samples|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.404|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.70E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.83E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.4|||||5.3|||||
ÍSOR-2011/064_170803-10|170803-10|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Silfurberg, north of Kögunarhóll|398243|385740|-21.07682|63.96008|78||Mjög ummynduđ túffreksía, misleitni möguleg á milli sýna. Breksían líklegast prímer. |Highly altered hyaloclasitie tuff breccia, possible heterogenity between samples, probably primary.|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.32|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.151|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.40E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.97E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.3|3.10||||68.0|||||
ÍSOR-2011/064_170803-11|170803-11|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Silfurberg, north of Kögunarhóll|398219|385771|-21.07733|63.96035|74||Um 5 m ofan viđ ummyndunina í sýni 10. Bresía sprungin og erfitt ađ taka heilleg sýni. Breksían líkelgast pr´mer ţar sem lagskipting er óljós. |Ca. 5 m above hydrothermal alteration, breccia fractured and sampling difficulties. Breccia probably primary as layering vague|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.48|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.153|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|6.62E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||8.56E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.9|4.15|||||||||
ÍSOR-2011/064_180803-01|180803-01|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut near Idntaeknistofnun|365481|406483|-21.76323|64.13476|56||Mjög ţétt túff, dökkt ađ lit sem líkelgast bendi til aukins magns fersks glers. . Brotgjarnt og sýnataka erfiđ. |Very compact tuff, dark in colour probably indicating high portion Unaltered glass. Heavily fractured and sampling difficult|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.43|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.254|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.19E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.49E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.5|3.35||||48.0|||||
ÍSOR-2011/064_180803-02|180803-02|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut near Idntaeknistofnun|365481|406483|-21.76323|64.13476|56||Brúnleit ummyndu viđ jađar jarđhitaćđar. Opal, chabasít ummyndun|Brownish alteration zone around hydrothermal fracture. Opal, chabazite alteration.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.293|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|7.28E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||8.21E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.85||||28.0|||||
ÍSOR-2011/064_180803-03|180803-03|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut in Mosfellsbaer|368696|409649|-21.70005|64.16438|63||Ráđandi túff, lagskipting óglögg. Halli laga um 45°NA. Útfellinga fátíđar nema í ćđum sjást kabasít og og kalsít.  Brúnleit ummydun viđ jađra sprugna, svipađ og finnst í sýninu nćrri Iđntćknistofnun. |Dominant tuff, layering not pronounced, inclination of layering 45°NE. Deposiiton not seen except in fractures (chabazite, calcite) and brownish alteration around veins similar to that found near Idntaeknistofnun (sample 18832).|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.45|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.216|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.45E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.82E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.3|3.60||||111.0|||||
ÍSOR-2011/064_180803-04|180803-04|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut in Mosfellsbaer|368764|409648|-21.69865|64.16440|60||Bólstraerg innan túff millimassa. Hvítar útfellingar í túffinu, sem er frábrugđiđ túffinu  fyrir ofan og líklegast takmarkađ palagonít.  |Pillow basalt embedded in tuff matrix. Tuff filled with white deposition, different from the overlying tuff, and probably with limited palagonitization |Pillow basalt|Pillow basalt|Smectite-zeolite|2.42|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.145|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.41E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.98E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|3.15||||41.0|||||
ÍSOR-2011/064_180803-05|180803-05|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut in Mosfellsbaer|368657|409674|-21.70087|64.16459|63||Sýni tekiđ norđan í vegkantinum.  Kjarninn brotgjarn og erfitt ađ taka sýni. Veđrun áberandi í yzta cm sem gefur vísbendingu um hrađa veđrunarinnar.  |Sample taken north part of roadcut. Fractured rock and difficult to get Boreholes. Weathering zone about 1 cm which gives an indication on rate of weathering.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.51|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.233|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.78E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.48E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.4|3.65||||64.0|||||
ÍSOR-2011/064_180803-06|180803-06|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut in Mosfellsbaer|368642|409675|-21.70118|64.16459|65||Lagskipt túff sem sést vel sunnan viđ veginn. Sýni tekiđ af 1 cm ţykkri ummyndađri sprungu. |Layered tuff as observed from exposures south of road. Sample taken from a 1 cm thick altered fracture. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite||||||||||||||||||||2.0|2.85|||||||||
ÍSOR-2011/064_190803-01|190803-01|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|Below dolerite north side of Kollafjordur|366610|414349|-21.74708|64.20569|16||lagskipt túff  setlag. Sýni tekiđ samsíđa laskiptingu. Lagiđ er tvískipt. Sýniđ tekiđ um 4 m neđan dólerít innskots. |Layered tuff conglomerate. Check whether tuff or not and select grainsize. Sample taken parallel to layering. Layer in two parts. Sample taken about 4 m below dolerite contact.  |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.80|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.260|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.82E-17|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||6.61E-17|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||3.0|3.30||||63.0|||||
ÍSOR-2011/064_190803-02|190803-02|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|Below dolerite north side of Kollafjordur|366610|414349|-21.74708|64.20569|16||Um 2 m neđan viđ dólerítiđ. Lagskipting í túffinu <5cm. Möguleg misleitni milli sýna, svo velja ţarf međ varúđ.|About 2 m below dolerite contact. Layering <5 cm. Possible grain size variation within samples, select with care. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.82|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.231|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.42E-18|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.96E-18|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||4.1|3.75||||99.0|||||
ÍSOR-2011/064_190803-03|190803-03|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Međalfell in Baejargil. |374698|426781|-21.59120|64.32017|169||Lagskipt túff á milli hraunlaga, rúnnun korna sést ekki, en afar líklegt ađ lagiđ sé setlag. Kornastćrđ <1cm, svo búast má viđ misleitni. Lagiđ amk. 1 m ađ ţykkt. Lagiđ er mun fínkornađra í neđri hlutanum er grófar er ofar kemur. Chabazite og analsím útfellingar sjást. |Layered tuff between lavaflows, rounding not visible but assumed to be reworked. grainsize <1 cm so heterogeneity expected. Layer at least 1 m thick. Layering finegrained near bottom but coarser grained on top. Chabazite, analcime alteration. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.52|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.268|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.00E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.06E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.1|3.20|||||||||
ÍSOR-2011/064_190803-04|190803-04|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Međalfell in Baejargil. |374751|426882|-21.59019|64.32110|211||6-8 m ţykkt túfflag, gróf lagskipting og bóstrabeg í efri hlutanum, en eitt samtíma lag. Verđur túffkennt um einum metra frá botni. |6-8 m thick tuff layer coarse layering and pillow basalt overlying but part of same formation, becomes tuff in the lowest 1 m from bottom. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite||||||||||||||||||||2.1|||||31.0|||||
ÍSOR-2011/064_190803-05|190803-05|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Međalfell in Baejargil. |374751|426882|-21.59019|64.32110|211||Lagskipt ljósbrúnt settúff. Athuga möguleika á misleitni á milli sýna.|Layered lightbrown tuff reworked. Note possibility of heterogeneity between samples. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.77|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.234|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.21E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.95E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||3.2|2.90||||48.0|||||
ÍSOR-2011/064_190803-06|190803-06|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Međalfell in Baejargil. |374755|426860|-21.59009|64.32090|207||Sýni tekin um 1-15 m neđan viđ efra borđ á 2-3 m ţykku settúffi. Lárétt lagskipting, setzt til í vatni, en engin skálaga setstrúktúr sést. Ljósbrúnt ađ lit.|Taken at about 1-15 m below upper boundary of a 2-3 m thick zone of reworked sedimentary tuff. Horizontal layering, water sorted, but no foreset bedding observed, lightbrown in colour and light-brown in colour. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.336|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.00E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.64E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.2|2.05|||||||||
ÍSOR-2011/064_200803-01|200803-01|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Miđfell|400998|411911|-21.03784|64.19551|152||Vestan viđ Thingvallavatn. Skálaga túffset blandađ bólstrum og breksíu. Halli laga um 32°og strik 30°.  Kornastćrđ <1cm, misleitni moguleg. Samlíming takmörkuđ svo útlínur kjarnans nokkuđ ójafn. |West side of Thingvallavatn lake.Foreset type of bedding with pillows in breccia. Dip of bedding about 32°and strike 30°. Grainsize less than 1 cm, heterogenity expected. Consolidation minimal with some erosion on the outside of Boreholes. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.334|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.94E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.86E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.25||||2.6|||||
ÍSOR-2011/064_200803-02|200803-02|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399739|414901|-21.06575|64.22195|189||Lítiđ lagskipt túff. Basaltmolar í túffinu upp í 5 cm.  Túffiđ fremur einsleitt. |Tuff with limited layering. Basalt fragments in tuff up to 5 cm in diameter. Tuff rather homogen. Sample taken out of a boalder that fell down from mountain. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.45|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.380|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.24E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.33E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.3|2.05||||7.6|||||
ÍSOR-2011/064_200803-03|200803-03|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399813|415069|-21.06434|64.22348|216|| skolvatniđ frá boruninni fremur oxađ fyrsta cm sem er vísbendingu um yfirborđsveđrunina. |Foreset tuff breccia, dip 30-40°towards east, rather coarse layering with fragments up to 5 cm in diameter. Samples has grainsize up to 1 cm . As is normal the water is more reddish and oxidized in the first 1cm of drilling. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.45|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.390|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.54E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.60E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.2|1.70||||6.1|||||
ÍSOR-2011/064_200803-04|200803-04|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399677|415100|-21.06716|64.22372|201||Nćrri toppi myndunarinnar. Lagskil halla um 10-20°, lagskil ekki samfelld, sem bendir til ađ lagiđ hafi orđiđ til ofan vatnsborđs. Kornastćrđ <1cm. |Near top of formation. Layering dipping 10-20°, layering discontinuous, i.e. Surface laid fragments. Fragment size less than 1 cm. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.72|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.346|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|7.64E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||7.72E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.20||||3.5|||||
ÍSOR-2011/064_200803-05|200803-05|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399672|415109|-21.06727|64.22380|198||Fínkorna og fínlagskipt túff innan sama lags og sýni 4 var tekiđ. Kjarni samsíđa lagskiptingu. Ţar nćrri er óreglulegur samtíma gangur, en ekki ber á aukningu á palagonitiserungu  nćrri ganginum. Sýnataka erfiđ vegna ónógrar samlímingar. |Fine grained and finely laminated tuff within the surface layer where sample 04 was taken. Sample taken parallel to layering. In that area an irregular dyke is observed. No apparent increase in palagonitization is observed, and sampling was not possible due to limited consolidation. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.66|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.447|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|5.81E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.92E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|2.05||||9.5|||||
ÍSOR-2011/064_200803-06|200803-06|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Tuff myndun viđ jađar á Reyđarbarmi-Kálfstinds móbergshrygg. Túffiđ fínkorna og vel samlímt. Kjarnar borađir samsíđa lagskiptingu. |A tuff sequence on the outside of Reyđarbarmur Kálfstindar hyaloclastite ridge. Sample of finegrained relatively compact tuff. Drilled parallel to layering. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.57|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.367|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.71E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.84E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|2.10||||12.0|||||
ÍSOR-2011/064_200803-07|200803-07|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Fremur einsleitt túff, dökkt og lagskipting ógreinileg. Borađ samsíđa lagskiptingu.|Relatively monotonous tuff, dark and layering not as definite. Drilled parallel to layering.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.463|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.54E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.50E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.5|||||20.0|||||
ÍSOR-2011/064_200803-08|200803-08|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Fínlaskipt túff < 2cm. Borađ samsíđa lagskiptingu|Finely layered tuff, layers less than 2 cm. Drilled parallel to layering|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.455|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.44E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.56E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7|1.85||||5.3|||||
ÍSOR-2011/064_200803-09|200803-09|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Fínlagskipt túff, brúnleitt, borađ ţvert á lagskiptingu. Kjarni vill springa, líklega vegna bólstrainnskota fyrir neđan.|Thin layered brown tuff, drilled perpendicular to layering. Some breakup of the tuff, probabley due to intrusive pillows which can be seen directly below. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.48|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.448|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.56E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.68E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.3|2.10||||9.7|||||
ÍSOR-2011/064_200803-10|200803-10|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Ţykka lagiđ í staflanum, erfitt ađ ná heillegum sýnum vegna takmarkađrar samlímingar. Handsýni tekiđ líka. Lagiđ er um 12 m ţykkt međ strjálum bólstrum inn á milli.|"The thick layer in the sequence, difficult to get samples due to limited consolidation. Hsnd speciamen also taken. Layer about 12 m thick with sparse ""intrusive"" pillows. "|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.78|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.461|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.39E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.25E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.3||||||||||
ÍSOR-2011/064_210803-01|210803-01|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|South end of Vörđufell|423378|394354|-20.56843|64.04381|77||Neđsta móbergiđ í Vörđufelli. Setkennt, og ađ hluta vatnslegiđ. Skálaga lagskipting sést. Ţykkt meira en 10 m. Lagiđ liggur undir hraunlagi. Virđist minna vatnsboriđ nćrri botni lagsins ţar sem vart verđur viđ bólstra breksíutopi lagsins. Kvarts ţóleiít.  Basalt laggangur í opnunni.|The lowest hyaloclastite found in Vörđufell. Reworked, and partly fluvial. Foreset fluvial bedding observed. Total thickness is more than 10 m. Overlain by lava. Appears to be less reworked near bottom where pillows can be found, but more fluvial near top. Tholeiitic composition of the hyaloclastite. About 0,5 m thick tholeiite sill is found in the exposure. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.172|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.52E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.09E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.9||||||||||
ÍSOR-2011/064_210803-02|210803-02|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|South end of Vörđufell|423390|394354|-20.56818|64.04382|77||Sýni tekiđ úr sama lagi en um 2 m neđar í opnunni. Sýnataka erfiđ vegna mikrósprungna. Hraunlag um 5 metrum ofar. |Same hyaloclastite be sample taken about 2 m lower in the hyaloclastite. Sampling difficult due to fine fracturing. Lava overlying about 5 m further up the sequence. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.46|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.241|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.28E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.60E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6||||||||||
ÍSOR-2011/064_210803-03|210803-03|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Reykholt Biskupstungur|430031|408496|-20.43888|64.17205|85||Árset, sandsteinskornastćrđ, skálaga. Liggur undir móberginu. |Fluvial sediment sandstone size, with foreset bedding. Underlies the hyaloclastite.|Sediment|Sediment|Smectite-zeolite|2.56|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.377|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.52E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.64E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.7||||||||||
ÍSOR-2011/064_210803-04|210803-04|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Reykholt Biskupstungur|430031|408496|-20.43888|64.17205|85||Ca. 15-20 cm ţykkt settúff, fínlagskipt, og nćrri sýnatökustađ 03.|Ca. 15-20 cm thick apparently reworked finely layered tuff, near to sample site 03. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.60|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.312|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.50E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.85E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.9|2.45|||||||||
ÍSOR-2011/064_210803-05|210803-05|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Reykholt Biskupstungur|430060|408528|-20.43830|64.17234|87||Um 15 cm ţykkt lagskipt túff, svipađ og sýni 04, líklegast setlag.  Vandrćđi í kjarnatöku vegna microsprungna. |"About  15 cm thick fine layered tuff similar to sample 04, probably reworked. Difficulties in getting samples due to microfracturing. Microfracturing possibly due to ""dry""fracturing. The overlying hyaloclastite is interesting as it appears to be partly subaerial with empedded  bombs. This is possibly an eruption in a water rich environment, and not necessarily a subglacial eruption. The formation is in general too coarse to sample, the south exposures have though to be checked. "|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.65|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.312|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|7.95E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.02E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|1.80||||10.8|||||
ÍSOR-2011/064_210803-06|210803-06|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Valahnúkar|460534|404132|-19.81055|64.13778|176||Engin lýsing tiltćk|No description given|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.62|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.334|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.38E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.71E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.3|2.75|||||||||
ÍSOR-2011/064_220803-02|220803-02|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar on Dómadalsroute|472698|397669|-19.55956|64.08099|386||Vestur hluti Valahnúks móbergs. Móberghryffur međ prímert túff, grófkennd lagskipting sem hallar 20-30°V, ađ ţví er virđist  gróf skriđa en ekki sést ísbending um tengsl viđ vatn|Western most part of the Valahnúkar hyaloclastite formation. Hyaloclastite ridge with a primary like tuff, coarse layering dipping about 20-30°W, apparently coarse avalances, but not water layering observed|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.55|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.348|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.92E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||9.35E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.2|2.60||||21.0|||||
ÍSOR-2011/064_220803-03|220803-03|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|472698|397669|-19.55956|64.08099|386||jökulset fyrir ofan skálagađs túffs, kornastćrđ minni en 0,5 cm, rúnnun korna sjáanleg. Sýni tekiđ efst í laginu sem er lárétt. Rof flötur neđan viđ. Sýni tekin samsíđa lagskiptingu. |Fluvial till above tuff with foreset bedding, grainsize less than 0,5 cm, rounding of pebbles observed, sample taken within the top part which is horizontally layered. Erosional boundary below. Sample taken parallel to laeyring. |Sediment|Sediment|Unaltered|2.58|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.250|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.42E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.54E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||3.0|3.30||||40.0|||||
ÍSOR-2011/064_220803-04|220803-04|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Túff neđan viđ síđasta sýni. Laghallo um 40° strikstefna  A. Sýni tekiđ samsíđa lagskiptingu. Kornastćrđ <1cm. Áhugavert ađ sjá meiri samlímingu ţar sem meiri sprungur er ađ sjá. |Tuff below sample 03. Dip about 40°Str. E. Sample taken parallel to layering. Grainsize less than 1 cm. Interesting to see more consolidation in the fine grained layers and in the more fractured part. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.349|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.62E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.73E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.9|2.40||||10.0|||||
ÍSOR-2011/064_220803-05|220803-05|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Sýni tekiđ ú ralgi sem hallar um 50° og er fremur grófkorna. Kornastćrđ <2cm, en ađ metu mun fínkornađra. |Sample taken from about 50°dipping coarsely layered tuff. Grainsize less thatn 2 cm. But mostly finer grained. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.87|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.398|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.24E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.29E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.0|2.50||||12.0|||||
ÍSOR-2011/064_220803-06|220803-06|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Sami stađ og síđasta sýni, en tekiđ úr mun fínkornađra túffi, halli 50°A og strik N-S. Ţetta er líklegt dćmi um flćđibrotflöt innan túffsins. |Same locality but taken from the finer grained tuff, dip 501E strike N-S. This is probably an example of friction flow planes within the tuff.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.62|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.336|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.26E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.32E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.2|2.80||||19.0|||||
ÍSOR-2011/064_220803-07|220803-07|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|475408|397095|-19.50393|64.07605|535||Sama svćđi en sýni tekiđ í grófari hluta túffsins, u.ţ.b. 20 m fjarlćgđ frá síđasta sýni, ţ.e. Innan flćđibrotflatar og svo utan hans. S+ýniđ er um 16 m frá sýni 05 og liggur neđan ţess. |Same locality taken from a coarser part of the tuff, about 20 cm from last sample, i.e. Sample from the friction plane and then from outside. Ca. 16 m from samplesite 05 and is underlying that  |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.64|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.348|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.00E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.08E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.0|2.55||||10.3|||||
ÍSOR-2011/064_220803-08|220803-08|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Krókagiljabrún SE of Lambafitjahraun|480581|395842|-19.39777|64.06514|568||lág og flöt móbergsmyndun. Gróf lagskipting, ekki sjást vísbendingar um áhrif frá vatni, mögulega myndun ofan vatnsborđs á gostíma. Hraunflyksur. Halli laga 5-10° í vesturátt. Sýni tekiđ rétt suđaustan Lambafitjahrauns. |Low and flat hyaloclasatite formation. Coarse layering, water action not observed, possibly sub-aerial part of formation. Magma patches, dip of layering 5-10°towards west. , Sample taken just southeast of the Lambafitjahraun.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.52|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.385|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.31E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.26E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|2.05||||13.0|||||
ÍSOR-2011/064_220803-09|220803-09|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Landmannahellishyaloclastite|480581|395842|-19.39777|64.06514|568||Sýni tekiđ á norđausturhliđ sömu móbergmyndunar og Landmannahellir er í. Grófkennd laskipting sem hallar 40-50° til norđurs. Líklega skálaga skriđa í vatni. |Sample taken in the NE side of hyaloclastite formation same as the Landmannahellir is in. Coarse layering dip 40-50°dippng N. Probable avalances into water|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.63|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.397|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.27E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.39E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.7|2.90||||26.0|||||
ÍSOR-2011/064_220803-10|220803-10|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Landmannahellishyaloclastite|488865|395071|-19.22803|64.05859|680||Um 20 cm túfflinsa í sömu breksíu og sýni 09 og í um 8 m fjarlćgđ. |A tuffrich lense, ca. 20 cm in same tuffbreccia as sample 09 and about 8 m away.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.60|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.406|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|9.35E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||9.13E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.1|2.50||||13.0|||||
ÍSOR-2011/064_220803-11|220803-11|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Hyaloclastite on left side before descending down into Dómadalur. |490403|391672|-19.19632|64.02815|604||Fremur grófkorna túff og međ grófa lagskiptingu  sem hallar um 30° međ strikstefnu NE-SW|Rather coarse grained tuff and coarsely layered, dips about 20°S, possibly near top of crater. Apparent preference of grains parallel to laeyringg.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.437|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.29E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.45E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.6|1.90||||8.9|||||
ÍSOR-2011/064_220803-12|220803-12|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Hyaloclastite west of Kirkjufellsós|503793|387450|-18.92252|63.99039|591||gróflagskipt túff, fremur fínkorna sem hllar um 30° međ strikstefnu NA-SW. |Coarse layered tuffs rather finegrained with dip of about 30°and striking NE-SW. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.72|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.374|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|9.50E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||8.13E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||1.8|1.95||||3.5|||||
ÍSOR-2011/064_220803-13|220803-13|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|River eroded exposure in to a hyaloclastite ridge|505040|386206|-18.89708|63.97922|610||Gróflagskipt túff . Kornastćrđ <1cm, virđist prímer. |Coarse layered tuff. Grainsize less than 1 cm, apears primary. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.59|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.211|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|7.44E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||9.55E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.4|3.10||||43.0|||||
ÍSOR-2011/064_220803-14|220803-14|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Hyaloclastite on north side of road, north of Tindafjalla|511416|386553|-18.76686|63.98218|679||Efst á móobergshrygg, nćr lárétt túfflag nokkuđ vel samlímt. |Top of a hyaloclastite ridge subhorizontal tuff layered, and relatively well consolidated. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.68|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.281|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.46E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.27E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||2.4|2.85||||28.3|||||
ÍSOR-2011/064_050903-01|050903-01|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|South end of Ţjórsárholt by river|441190|392432|-20.20318|64.03008|132||Um 18 m ţykkt túff set. Efri hlutinn er völuberg, en neđri hlutinn fínkornađra međ grófari linsum inn á milli sýni tekiđ í leirlagi um 1-2 m neđan viđ grófa lagiđlagiđ er mislćgt viđ hraunlagiđ sem ofan á liggur. 'opall og kalsít útfeyllingar|A total of about 18 m thick sediment. Upper part conglomerate, lower 8 m finer grained with coarser intercalated lenses. Sample taken in a silty layer about 1-2 m below the boundary of the coarse layer. An erosional unconformity is between the overlying lava and the sediment.  Opal and calcite found in the sediment. |Hyaloclastite|Hyaloclastite sediment|Unaltered|2.62|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.254|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.52E-17|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||6.12E-17|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_050903-02|050903-02|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|Ca. 1 km east of Gaukshöfđi and about 2 m from main road|451712|399404|-19.99018|64.09425|133||rúmlega sex metra ţykkt túff árset, međ breytilegri kornastćrđ. Lagiđ sem sýniđ var tekiđ úr er <1m ţykkt og er lárétt og fíkorna. Roflćnur sjást í setinu rétt ofan viđ sýnatökusađinn. |>6 m thick river tuff sediment, variable grainsize. The layer from which the sample is taken  is <1 m thick, is ~horizontal layering and fine grained.  Erosional channel observed in the sediment ust above the fine grained sample layer.  |Hyaloclastite|Hyaloclastite sediment|Unaltered|2.48|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.457|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.66E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.39E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_050903-03|050903-03|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|Gaukshöfdi, in roadcut|451712|399404|-19.99018|64.09425|133||Túfflag neđan viđ bólstraberg, líklegt basalt lag sem tilheyrir ţessari myndun. Ferskt gler, palagonít međ takmörkuđum poruhluta. Thomsonít, analsím, chabasít og opal útfellingar. |A tufflayer below pillow basalt, probably a basalt layer of that formation. Unaltered glass, palagonite, and minor porosity. Thomsonite, analcime, chabazite and opal.|Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.42|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.122|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|6.59E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||8.52E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_050903-04|050903-04|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|Gaukshöfdi, in roadcut a few meters west of sample 5933|450632|397989|-20.01186|64.08140|148||Gráleitt , ţétt og leirkennt set međ molum upp ađ 40cm. Sýni tekiđ úr fína hlutanum, lagskipting sést illa. Gćti veriđ leirflóđ. |Greyish, tight and silty sediment with individual boulders up to 40 cm in diameter. Sample taken from the fine grained part. Layering hardly visible, possibly a mudflow.|Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.86|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.227|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.14E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.18E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_050903-05|050903-05|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|Road cut about 5-1 m east of Fossá|445980|396091|-20.10651|64.06368|122||Túffríkt rýţmískt árset. Fínkorna međ stćrri molum (<5cm) inn á milli. Roflćnur sjás innan setsins og rúnnun setkorna. Sýniđ tekiđ innan fínkornađasta hluta lagsins. |Tuff-rich rythmic river sediment.  Interstitial coarse (<5 cm) and fine grained sediment. Erosional river channels observed and rounding of pebbles. Sample taken from fine grained silty part. |Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.43|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.284|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.94E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.98E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-01|120903-01|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|Sediment west of Fossá|445436|395828|-20.11756|64.06124|119||Túffset, sýnataka nćr ómöguleg vegna mikrósprungna sem brotna í borun. |Tuff sediment, sampling near impossible due to microfracturing of samples during drilling. |Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.46|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.197|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.10E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.44E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-02|120903-02|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|West side of Reykholt, smooth surfaced  hyaloclastite|458437|404755|-19.85378|64.14312|160||Líklega prímert túff, kúlur sjáanlegar (accretionary lapilli) sem eru <2cm, óglögg lagskipting, sér sýni tekiđ af kúlunum. Úr lagi 14 í IBF et al. |Probably primary tuff, spherules observed (<2 cm), layering insignificant, separate sample taken of spherules.  From unit 14 in IBF et al.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.64|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.269|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.92E-17|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.47E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-03|120903-03|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|West side of Reykholt same hyaloclastite as 12932|458745|405260|-19.84759|64.14769|160||Túff međ ógreinilegri lagskiptingu, líklegast prímer, útfellingar algengar, sýni úr lagi 14 í IBF et al. |Tuff, insignificant layering, probably primary, amygdales common, from unit 14 in IBF et al.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.37|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.104|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.54E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.99E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-04|120903-04|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|West side of Reykholt same hyaloclastite as 12933|459165|406165|-19.83921|64.15585|160||Túff, lagskipting ógreinileg og líkega prímert túff. Möguleg rúnnun samt sem einkenni sets sem ćtti ađ sjást í ţunnsneiđargreiningu. Sýnataka erfiđ vegna mikrósprungna. Opal fyllingar mögulega. |Tuff, insignificant layering, probably primary, but possible rounding and reworked origin may be evidenced in thin section. Sampling difficult due to fracturing.  Filling possibly silia. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.30|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.145|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.94E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.98E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-05|120903-05|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|E-Thjorsárdalur|459583|406791|-19.83079|64.16152|160||Tuúff međ ógreinilega lagskiptingu, líklega prímer. Fíkorna ´tuff međ g´rofari lögum inn á milli. Opnan er um 20 m ţykk og fyrir ofan er bólstraberg sem er hluti sömu myndunar.  Fallegir kjarnar. Opal og fleiri úfellingar . |Tuff with limited layering, probably primary. Fine tuff with intecalated coarser tuffs. Exposure about 20 m thick and above is a pillowbasalt belonging to same formation. Good coring. Opalline and other amygdales. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.49|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.232|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.38E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.98E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_120903-06|120903-06|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|At north end of Reykholt, ca, 1 west of Swimmingpool.|460105|406936|-19.82010|64.16288|166||Líklegat prímert túff međ ógreinilegri lagskiptingu. Útfellingar algengar svo sem kalsít og stílbít. |Probably primary tuff with limited layering, fillings comon like calcite and stilbite. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.42|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.103|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.37E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.52E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_230903-01|230903-01|Franzson et al., 2011|Frolova et al., 2005|23.9.2003|Surface|"NE-end of Thjorsárdalur on way to ""summer house"" there"|458264|408138|-19.85828|64.17344|196||Prímert nćr ólagskipt túff međ nokkurri misleitni. Ólivín ţóleiite gangur sker túffiđ og hefur strikstefnu 310°.  Um 4 m ţykkt ummyndunarbelti er fram međ ganginum berandi vitni um jarđhitaummyndun. Sprungustefnur 30 og 80°. Bólstraberg í grennd. Ummyndunarsteindir kalsít, skólesít og stilbít. kjranataka erfiđ vegna míkrosprungna. Oxun í sprungum vísbending um kalt grunnvatnsstreymi. |Primary near unlayered tuff, somewhat heterogeneous. A  olivine tholeiite dyke cuts through the tuff striking 310°. About 4 m wide alteration zone around the dyke indicating hydrothermal permeability and alteration. Fracture pattern 30°and 80°. Pillow basalt near to the tuff. Alteration minerals calcite, scolecite, stilbite. Coring difficult due to fracturing. Fractures often oxidized (Surface effect or coldwater infiltration)|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.35|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.095|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.09E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.53E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_291004-01|291004-01|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarđ in Hengill|383694|394600|-21.38030|64.03490|341||Sýni úr ferska hluta túffsins. Ummyndun sjáanleg í túffinu en virđist einskorđast viđ sprungurnar.|Sample taken from the Unaltered part of tuff. Hydrothermal alteration is visible in the tuff around fractures.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.54|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.269|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|6.77E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||8.73E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_291004-02|291004-02|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarđ in Hengill|383695|394610|-21.38029|64.03499|341||Ummynađ túff, ţótt ekki sjáist til útfellinga. Laghalli um 30Ĺ og strik um 30°. |Altered tuff without visible alteration deposition. Layering dips about 30°E and strikes 30°.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.50|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.460|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.49E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.60E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_291004-03|291004-03|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarđ in Hengill|383692|394622|-21.38036|64.03510|341||Fremur grófkorna túff, lagskipting svipuđ og í sýni 29100402. Hvítleitar útfellingar. |Relatively coarse grained tuff, layered as in previous sample of 29100402. contains whitish deposition minerals.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.44|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.419|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.61E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.10E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_291004-04|291004-04|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarđ in Hengill|383682|394638|-21.38058|64.03524|338||Dökkgrátt, mjög fínkorna og ţétt túff. Ţetta túff eru hnullungar um 30 cm í ţvermál innan brúna túffsins og mögulegar framandsteinar. |"Dark gray, very fine grained and dense tuff. This tuff are boulders of ca. 30 cm diameter within the brown tuff, possibly ""xenoliths"". "|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.50|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.379|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.28E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.35E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-01|011104-01|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|Easternmost Arnarthufa, west of Vifilfell|373648|396762|-21.58749|64.05074|181||Austast í Arnarţúfu vestur af Vífilfelli. Lítil túffnáma. Túffiđ er illa lagskipt og líklega prímert. Túffiđ er einsleitt og fínkorna.|Easternmost Arnarthufa, west of Vifilfell. A small tuff quarry. Tuff is badly layered and probebly primary, tuff relatively homogeneous and fine grained.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.57|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.353|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.92E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||9.35E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-02|011104-02|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|Southwest end of Raudhnukar at Bláfjalla- and Hafnarfjardarroad intersection.|371079|392631|-21.63651|64.01277|411||"Sýni úr fínkorna líklega prímeru fínlagskiptu  túffi. Sýniđ er tekiđ frá líklegri gosrás túffsins. Laghallinn er <30° og gćti veriđ ""base surge"". "|Sample taken from a finelayered tuff, appears to be primary, but could be from the layered part. The sample is taken near to proposed vent of the formation. Layering dipping less than30°, and could be base surge. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.62|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.457|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.48E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.57E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-04|011104-04|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|Sandfell in Ţrengsli, west side. Slightly north and above the quarry.|379083|386078|-21.46777|63.95693|245||Sýniđ tekiđ innan illa lagskipts túffs, međ tiltölulega misleitna kornastćrđ, og líklegast prímer. Mjög fínlagskipt túff (mögulega ţekja af jökulkyni) liggur ofan á túffinu og hallar 30°međ strikstefnu 60°. Túffiđ getur veriđ ţetta týpíska túffţekja sem liggur ofan á bósltrabergi. |"Sample taken within partially layered tuff, relatively heterogeneously grained, and possibly primary. Very finely layered tuff (possibly glacially relatied  coating of the hyaloclastite) lying directly above the sample point. layering dipping 30°NE and striing 60°. THis layer could be a typical ""tuff coat"" around pillow basalt."|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.68|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.335|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.39E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.48E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-06|011104-06|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|Probably NE of Einbúi on south side of Reykjanes west of Krísuvík road|347893|377402|-22.09475|63.86688|124||Tiltölulega grófkorna túff. Meiri samlíming túffsins í kringum sprungur.  Algengt ađ sjá móbergshlunka sem snúist hafa innan túffmassans. Lagskil innan túffsins fremur óregluleg (líklegast vegna snúnings hlunkanna).|Realtively coarsegrained tuff. More hardened fractures seen in tuff. Rotated blocks common, layering irregular (probably because of block rotation).|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.398|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.21E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.26E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-08|011104-08|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|South part of Vigdísarvellir road, possibly NE part of Tófubruna hyaloclastite|342596|376842|-22.20176|63.85950|99||fín lagskipt túff innan prímerrar breksíu. Sýnin tekin ţvert á lagskiptingu|Fine layered tuff within primary primary breccia. Sample taken perpendicular to layering. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.76|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.405|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.25E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.23E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-09|011104-09|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|South part of Vigdísarvellir road |344214|378426|-22.17052|63.87442|138||Opna í túff inn í skriđu vinstra meginn viđ veginn, um 50 m frá, líklegast í norđaustur hluta Tófubruna hrygg. Lagskil óveruleg. Líklegast prímert, og róterađir  móbergshlunkar sjást. |Tuff exposure within scree on left side of road, at a distance of about 50 m, probably in northeast part of Tófubruni ridge. Tuff limited layering, possibly primay, layering irregular and blocks probably rotated. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.57|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.392|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.00E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.05E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_011104-10|011104-10|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|South part of Vigdísarvellir road about 3 m from road|344989|378700|-22.15505|63.87722|126||Prímert túff, ógreinileg lagskipting. Frekar gróft. Ţarf ađ tékka misleitni milli kjarna. |Primary tuff, vague layering. Tuff relatively coarse, check heterogeneity. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.67|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.366|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.48E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.55E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-01|021104-01|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|North end of Vigdísarvellir track|355324|388553|-21.95438|63.96998|139||Fyrsta móbergiđ til hćgri á norđurenda Vigdísarvallavegi. Prímert túff, fremur fínkorna inn á milli grófara túffs. Lagskipting ógreinileg. Móbergshlunkar međ snúningi. |First hyaloclastite on right side on north end of Vigdísarvellir track. Primary tuff, relatively finegrained among coarser ones. Layering not distinct. Rotated blocks within tuff. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.69|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.334|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.58E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.08E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-02|021104-02|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|355059|388171|-21.95941|63.96644|161||Fínkorna túffvel samlímt, grábrúnt, líklegast pakkađ međ jökulleir. Borađ ţvert á lagskiptingu. Strik 60°halli 30°NV|Fine layered hard, brownish gray, probably surface glacially packed. Drilled perpendicular to layering. Strike 60°dip 30NW|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.67|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.221|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.46E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.59E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-03|021104-03|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|354299|387249|-21.97402|63.95786|210||Sýni tekiđ ţar sem vegurinn sveigir upp brekkuna. Prímert túff. Ógreinieg lagskilsamlíming virđist meiri viđ sprungur. |Sample taken just before road sways upphill. Primary tuff. Layering insignificant. Fractures more consolidated. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.66|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.377|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.82E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.94E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-04|021104-04|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|353925|387299|-21.98170|63.95815|195||Prímert túff sýni tekiđ nćrri vegi lengra til suđausturs. Tékka ţarf á misleitni milli kjarna. Fínlagskiptari túff inn á milli (sem oft má sjá í ţessari túffgerđ. Ţessi lög eru oft hreyfđ, sem bendir til hreyfingar á túffinu međan á gosi stendur. |Along same tack to southeast. Primary tuff, heterogeneity needs to be checked. More finely layered tuff layers observed within the primary tufflayeres (often seen in primary tuffs). These layers are often disturbed indicating movement of the partially unconsolidated hyaloclastite during the eruption. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.66|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.441|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.90E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||7.64E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-05|021104-05|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|353738|387147|-21.98536|63.95671|216||"Lagskipt túff nćrri vegi lengra í suđaustur. Líklegast ""skriđa í vatni"". Lagţykkt <20 cm. Mćtti ađgćta val á kjörnum til samrćmis. Nokkur oxun. Lögin halla um 20° og međ strikstefnu 50°. Sýni tekiđ um 20 m ofan vegar og nćrri botni 30 m ţykks túfflags. skriđueinkenni ekki til stađar, ţ.e. ađ lagiđ heldur jafnri 10 m ţykkt um 10 m. mögulea sama lag og sýni 04 ađ ţví undanskyldu ađ ţađ er vel lagskipt. "|Along same track to southeast. Layered tuff probably base surge. Layering <20 cm, check selection of Boreholes. Somewhat oxidized. Layering strikes 50°and dips 20°NW. Sample taken ca 20 m from road an at the bottom of a 30 m thick layered tuff. Base surge erosion not notable, i.e. layering with equal thicknesses over more than 10 m. possibly same formation as sample 04, except it is well layered. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.61|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.321|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.96E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.11E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-06|021104-06|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|351695|384777|-22.02468|63.93461|251||Líklegast samanlag og sýni 04 og 05. gróf lagskipt (<0,5 m), líklegast prímert. Sýni tekiđ hornrétt á lagskiptinguna.  Áhugavert ađ ekkert bólstraberg finnst innan myndunarinnar.|Probably same hyaloclastite as last two samples (04, 05). Coarsely layered (<0,5m) probably primary, sample taken perpendicular to layering (not important). Interesting that no pillow basalt is senn in this formation. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.438|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.62E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||4.74E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-08|021104-08|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Reykjanes high temperature field, southwall of excavated drillpad for RN-18|319029|374394|-22.67723|63.82608|29||mjög ummyndađ ljósleitt túff, allt gler ummyndađ, afar leirríkt. |Highly altered light colour tuff, all glass disappeared. Highly clayish. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.46|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.374|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.06E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.11E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_021104-09|021104-09|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Reykjanes high temperature field|319298|374597|-22.67202|63.82804|32||Sama móbergsmyndun og sýni 08, en sýni tekiđ um 100 m norđaustan viđ veginn.  Prímert túff, sýni frekar misleit og ţarf ađ athuga frekar. Oxun áberandi. |Same hyalolastite formation as sample 08, but located about 100 m northeast of road. . Primary tuff, relatively heterogeneous-smples need checking, oxidation prominent.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.48|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.494|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|6.76E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||6.86E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_031104-01|031104-01|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Southeast side of Blákollur|378871|395205|-21.47940|64.03866|354||Fremur illa lagskipt túff. Sýni tekin ţar sem ţađ er mest fínkorna. Lagskil hallar um 20° en óreglulega. Túff telst vera prímert en mćtti endurskođa, gćti veriđ lagskipta týpan. |Rather coarse layering. Sample taken from relatively finegrained part. Layering dipping less than 20° but irregular. Tuff termed primary but could be reconsidered as the layered type..   |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.75|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.412|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|9.11E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||7.82E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_031104-02|031104-02|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Southeast side of Blákollur|378923|395276|-21.47839|64.03932|352||Skriđukenndur rofflötur fyrir ofan sýnatökustađ ţar sem túffiđ er mun betur lagskipt (ca. 5-6 m) og var sýni tekiđ ţar ţar sem ţykkt laga er <2cm. Ţar fyrir ofan er túffiđ veđur mun grófara og minna lagskipt, sem bendir til aukinnar gosvirkni. Halli laga er um 1°. fjarlćgđ sýnis er um 100 m frá gosrás. |Above the sample point base surge erosional surfaces noted where tuff is much better layered (a. 5-6 m thick) sample taken there. layering < 2 cm. Above that coarse grained and less layered tuff occurs again (which indicates increasderuptive intensity). Dip of layering 1°N and strike 120°. sample taken within 100 m from eruptive vent. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.59|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.400|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|8.67E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||9.68E-14|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_031104-04|031104-04|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Ingólfsfjall quarry|399360|385878|-21.05413|63.96164|180||Sýni tekiđ um 10 m vestan sýnis 03. Áhugavert ađ sjá ađ túffiđ er lárétt eins og lárétt hraun sem liggja ofan á túffinu bera međ sér. |Sample taken about 10 m to the west of sample 03. Interesting that the top of the hyaloclastite is flat as evidenced by the extensive lavaseries above that. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.43|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.181|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|9.59E-16|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.38E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_031104-06|031104-06|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Southeast corner of Ţingvallavatn|401787|404952|-21.01704|64.13335|102||Móbergsmyndun viđ suđaustur horn Ţingvallavatns. Hallandi lagskil greinanleg. Sýni tekiđ innan frekar fíngerđs túffs, en grófari breksía ţa fyrir ofan. |Recent hyaloclastite at southeast corner of Thingvallavatn. Layering visible and subhorizontal. Taken from a relatively fine grained tuff, but coarser breccia above.  |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.67|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.282|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.97E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.06E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_HE-01|HE-01|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|435931|327114|-20.28361|63.44341|29||"Heimaey. Skipahellir. Loftboriđ túff međ bombu gígum og ""accretionary lapilli"".  Utan gígsvćđis. Strik 0° halli 50°. Berg vel samlímt. "|Heimaey. Skipahellir. Airfall tuff with accertionary lapilli and bombsag. On outside part of crater. Strike >0° dip 50 S. Rock very hard.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.56|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.375|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.40E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.51E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_HE-02|HE-02|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|436724|327479|-20.26787|63.44682|23||Heimaey, Heimaklettur. Prímert túff, lagskil vart sjáanleg. |Heimaey. Heimaklettur. Primary tuff (chaotic tuff) Layering vaque|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.53|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.388|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.01E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.11E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_HE-03|HE-03|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|436715|323479|-20.26645|63.41095|36||Heimaey. Toppur á Sćfelli sem er 6000 ára. Surtseyjar gosstíll. Einhver palagonitisering í túffinu. Lögins halla 16°međ 60° strikstefnu. |Heimaey. Topp of Sćfell 6000 yrs. A Surtseyan eruption. Mildly palagonitised tuff. Layers strike 60° dip 16°S. Bomb sags conspicuos. |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.415|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|2.32E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||2.41E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_HE-04|HE-04|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|436491|323073|-20.27077|63.40727|51||Heimaey. Neđsti hluti Sćfells sem er 6000 ára. Mjög palagonitiserađ lagskipt túff. Lítt hallandi lagskipting. Palagónitiseringin líklegast vegna jarđhitaflćđis frá gosstöđinni. |Heimaey. Bottom of Sćfell 6000yrs. Highly palagonitized. Layered tuff. Subhorizontal layering. Palagonization probably due to geothermal outflow from eruption vent.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.72|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.352|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|3.45E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||3.56E-12|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_SU-03|SU-03|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Surtsey|419792|311829|-20.59908|63.30306|103||"Surtsey. Vel samlímt loftboriđ túff. Lagskipt, ""Accretionary lapilli"". Lagskilin halla inn í gíginn. "|Surtsey. Hard palagonized airfall tuff. Layered, Accretionary lappili. Layering shallow dipping into crater.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.70|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.345|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|4.18E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||5.54E-15|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_SU-05|SU-05|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Surtsey|419680|311957|-20.60138|63.30418|105||"Surtseyjarđhitasprunga međ 95°strikstefnu. ""accretionary lapilli"". Oxun. Strik lagskila 80° en eru lítt hallandi. "|Surtsey. Geothermal fracture with 95° strike. Accretionary lappili. Crust oxidation. Fracture strike 80°. Layering near horizontal|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.54|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.467|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.21E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.20E-11|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
ÍSOR-2011/064_Helgafell|Helgafell|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Helgafell near Hafnafjörđur|547268|495824|-17.99944|64.95919|842||Nćr lárétt túff á toppi Helgafells. |Flat layered tuff on top of Helgafell |Hyaloclastite|Hyaloclastite tuff|Unaltered|2.58|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||0.340|He Gas pycnometry, Orkustofnun; additional data using air pycnometry was collected by J. Frolova (see paper)|1.57E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).|||1.70E-13|Measured by Julia Frolova in Russia, according to State Standard of Russian Federation (1985).||||||||||||||||||
BUĐARHALS_1|1|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.90|Triple-weight|||0.08|Triple-weight|||||||||||||||||||89.4|15.2||||
BUĐARHALS_2|2|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.10|Triple-weight|||||||||||||||||||94.2|15.5||||
BUĐARHALS_3|3|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.86|Triple-weight|||0.10|Triple-weight|||||||||||||||||||78.6|17.7||||
BUĐARHALS_4|4|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt, blođrött efst en ţéttist er neđar dregur (1%). Blöđrur yfirleitt međ holufyllingum. |Altered Olivine Tholeiite: vesicular at the top but more compact lower down (1%). Filled vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.08|Triple-weight|||||||||||||||||||79.3|22.1||||
BUĐARHALS_5|5|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|210|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.91|Triple-weight|||0.11|Triple-weight|||||||||||||||||||55.5|18.7||||
BUĐARHALS_6|7|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt, blođrött efst en ţéttist er neđar dregur (1%). Blöđrur yfirleitt međ holufyllingum. |Altered Olivine Tholeiite: vesicular at the top but more compact lower down (1%). Filled vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.10|Triple-weight|||||||||||||||||||48.2|17.7||||
BUĐARHALS_7|8|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.94|Triple-weight|||0.09|Triple-weight||||||||||||||||||0.2|93.5|43.5||||
BUĐARHALS_8|9|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple-weight|||0.08|Triple-weight|||||||||||||||||||91.4|25.0||||
BUĐARHALS_9|10|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.94|Triple-weight|||0.09|Triple-weight|||||||||||||||||||65.0|13.2||||
BUĐARHALS_10|11|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|193|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.90|Triple-weight|||0.19|Triple-weight|||||||||||||||||||7.6|1.4||||
BUĐARHALS_11|12|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|192|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.86|Triple-weight|||0.21|Triple-weight|||||||||||||||||||9.3|2.8||||
BUĐARHALS_12|13|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt, blođrött efst en ţéttist er neđar dregur (1%). Blöđrur yfirleitt međ holufyllingum. |Altered Olivine Tholeiite: vesicular at the top but more compact lower down (1%). Filled vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.07|Triple-weight|||||||||||||||||||80.7|21.4||||
BUĐARHALS_13|14|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt, blođrött efst en ţéttist er neđar dregur (1%). Blöđrur yfirleitt međ holufyllingum. |Altered Olivine Tholeiite: vesicular at the top but more compact lower down (1%). Filled vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.94|Triple-weight|||0.08|Triple-weight|||||||||||||||||||78.6|21.9||||
BUĐARHALS_14|15|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|85|Basalt: ljósgrátt, fínkornótt. Smádilótt, plag. (2-4%). Ţétt en nokkrar smáblöđrur og finblöđruband. Fersk og óhlufyllt. Ljós leir og siltsteinn ó spr. Fl.|Tholeiite, light grey, small vesicles, rather fresh with some brown clay.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|3.04|Triple-weight|||0.06|Triple-weight|||||||||||||||||||135.7|13.2||||
BUĐARHALS_15|16|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|85|Basalt: ljósgrátt, fínkornótt. Smádilótt, plag. (2-4%). Ţétt en nokkrar smáblöđrur og finblöđruband. Fersk og óhlufyllt. Ljós leir og siltsteinn ó spr. Fl.|Tholeiite, light grey, small vesicles, rather fresh with some brown clay.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|3.02|Triple-weight|||0.05|Triple-weight|||||||||||||||||||146.6|14.2||||
BUĐARHALS_16|18|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|189|Sandsteinsvöluberg: vel samt og heillegt. Grćnleitur. Sand- og siltboriđ. Nungr. Völur (grofa-möl). Heillt skeni á sprungur flötum. Sumastađar 3-4 mm fyllingar af hvitum og grćnl. Leir á skástigum spr. Fl.|Sandstone, sand and silt containing. Some precipitates. |Sediment|Sediment|Smectite-zeolite|2.87|Triple-weight|||0.23|Triple-weight|||||||||||||||||||33.3|6.0||||
BUĐARHALS_17|19|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|194|Sand-siltsteinn (ummyndađ): Hvarfleir-stöđuvatnasel. Logrétt lagskipt skiptast á greni sandst. Međ völum og illa samlimdur rauđi sillst. Liklega öll nokkuđ ummyndađ.|Sandstone, horizontal layering, mostly altered. |Sediment|Sediment|Smectite-zeolite|2.90|Triple-weight|||0.24|Triple-weight|||||||||||||||||||35.4|6.9||||
BUĐARHALS_18|20|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|194|Sand-siltsteinn (ummyndađ): Hvarfleir-stöđuvatnasel. Logrétt lagskipt skiptast á greni sandst. Međ völum og illa samlimdur rauđi sillst. Liklega öll nokkuđ ummyndađ.|Sandstone, horizontal layering, mostly altered. |Sediment|Sediment|Smectite-zeolite|2.96|Triple-weight|||0.24|Triple-weight|||||||||||||||||||34.7|6.4||||
BUĐARHALS_19|21|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.94|Triple-weight|||0.29|Triple-weight|||||||||||||||||||18.2|5.2||||
BUĐARHALS_20|22|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|8|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.59|Triple-weight|||0.08|Triple-weight|||||||||||||||||||125.2|22.6||||
BUĐARHALS_21|23|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.58|Triple-weight|||0.20|Triple-weight||||||||||||||||||0.2|52.4|17.0||||
BUĐARHALS_22|25|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|42|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.58|Triple-weight|||0.23|Triple-weight|||||||||||||||||||16.8|5.4||||
BUĐARHALS_23|26|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|39|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.57|Triple-weight|||0.22|Triple-weight|||||||||||||||||||24.3|6.0||||
BUĐARHALS_24|27|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.59|Triple-weight|||0.32|Triple-weight|||||||||||||||||||7.1|3.1||||
BUĐARHALS_25|28|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|39|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.57|Triple-weight|||0.26|Triple-weight|||||||||||||||||||28.3|7.6||||
BUĐARHALS_26|29|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.60|Triple-weight|||0.29|Triple-weight|||||||||||||||||||8.8|3.5||||
BUĐARHALS_27|30|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|42|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.61|Triple-weight|||0.28|Triple-weight|||||||||||||||||||9.0|3.7||||
BUĐARHALS_28|31|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.58|Triple-weight|||0.31|Triple-weight|||||||||||||||||||8.9|3.4||||
BUĐARHALS_29|32|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|42|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.58|Triple-weight|||0.27|Triple-weight|||||||||||||||||||19.0|5.8||||
BUĐARHALS_30|33|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|31|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.59|Triple-weight|||0.26|Triple-weight||||||||||||||||||0.2|36.0|11.8||||
BUĐARHALS_31|34|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|8|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.62|Triple-weight|||0.09|Triple-weight|||||||||||||||||||116.2|27.1||||
BUĐARHALS_32|35|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|8|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.58|Triple-weight|||0.08|Triple-weight|||||||||||||||||||135.6|11.5||||
BUĐARHALS_33|36|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|193|Sand-siltsteinn (ummyndađ): Hvarfleir-stöđuvatnasel. Logrétt lagskipt skiptast á greni sandst. Međ völum og illa samlimdur rauđi sillst. Liklega öll nokkuđ ummyndađ.|Sandstone, horizontal layering, mostly altered. |Sediment|Sediment|Smectite-zeolite|2.91|Triple-weight|||0.24|Triple-weight|||||||||||||||||||32.7|7.4||||
BUĐARHALS_34|37|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.93|Triple-weight|||0.24|Triple-weight|||||||||||||||||||19.1|6.9||||
BUĐARHALS_35|38|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.92|Triple-weight|||0.27|Triple-weight|||||||||||||||||||10.7|4.2||||
BUĐARHALS_36|39|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.99|Triple-weight|||0.23|Triple-weight||||||||||||||||||0.1|39.4|16.1||||
BUĐARHALS_37|40|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.97|Triple-weight|||0.26|Triple-weight|||||||||||||||||||20.7|7.2||||
BUĐARHALS_38|41|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.93|Triple-weight|||0.28|Triple-weight|||||||||||||||||||11.5|3.3||||
BUĐARHALS_39|42|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.93|Triple-weight|||0.09|Triple-weight||||||||||||||||||||||8.5||
BUĐARHALS_40|43|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.91|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||8.7||
BUĐARHALS_41|44|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|122|Basalt: dulk, dökkgrátt, Plagioklasdílott (2-4%). Mjög blöđrótt, stórar bl. og holrými. Einnig smábl. B-nd. Fersk og lit holufyllt. Eitthvađ ljósbrunum og gulleitu silti eđa leir. Stuđlasprungur og ţverspr. Spr. Fl. Orl. Skendir, ljósbrúnn leir. |Tholeiite (Vesicular). Plagioclase porphyry. Some dark brown or yellowish clay. |Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.91|Triple-weight|||0.09|Triple-weight||||||||||||||||||||||6.6||
BUĐARHALS_42|45|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt, blođrött efst en ţéttist er neđar dregur (1%). Blöđrur yfirleitt međ holufyllingum. |Altered Olivine Tholeiite: vesicular at the top but more compact lower down (1%). Filled vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||5.9||
BUĐARHALS_43|46|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.90|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||8.4||
BUĐARHALS_44|47|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||7.1||
BUĐARHALS_45|48|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.09|Triple-weight||||||||||||||||||||||7.1||
BUĐARHALS_46|49|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|214|Olivínbasalt (ummyndađ): smákornótt (0.5-2 mm). Ţétt, dökkgrćnt. Grćni fylingar af kristalluđu efni á fl Stuđlasprun. Og sumast. Sundursođiđ.|Altered Olivine Tholeiite, fine-grained, compact, dark-green alteration. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.92|Triple-weight|||0.09|Triple-weight||||||||||||||||||||||9.0||
BUĐARHALS_47|50|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|210|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.91|Triple-weight|||0.10|Triple-weight||||||||||||||||||||||2.8||
BUĐARHALS_48|51|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|210|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.90|Triple-weight|||0.11|Triple-weight||||||||||||||||||||||5.5||
BUĐARHALS_49|52|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|210|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.91|Triple-weight|||0.13|Triple-weight||||||||||||||||||||||3.6||
BUĐARHALS_50|53|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|193|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.88|Triple-weight|||0.14|Triple-weight||||||||||||||||||||||0.9||
BUĐARHALS_51|54|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|189|Sandsteinsvöluberg: vel samt og heillegt. Grćnleitur. Sand- og siltboriđ. Nungr. Völur (grofa-möl). Heillt skeni á sprungur flötum. Sumastađar 3-4 mm fyllingar af hvitum og grćnl. Leir á skástigum spr. Fl.|Sandstone, sand and silt containing. Some precipitates. |Sediment|Sediment|Smectite-zeolite|2.88|Triple-weight|||0.22|Triple-weight||||||||||||||||||||||3.5||
BUĐARHALS_52|55|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|189|Sandsteinsvöluberg: vel samt og heillegt. Grćnleitur. Sand- og siltboriđ. Nungr. Völur (grofa-möl). Heillt skeni á sprungur flötum. Sumastađar 3-4 mm fyllingar af hvitum og grćnl. Leir á skástigum spr. Fl.|Sandstone, sand and silt containing. Some precipitates. |Sediment|Sediment|Smectite-zeolite|2.93|Triple-weight|||0.26|Triple-weight||||||||||||||||||||||3.1||
BUĐARHALS_53|56|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.85|Triple-weight|||0.21|Triple-weight||||||||||||||||||||||2.6||
BUĐARHALS_54|57|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|189|Sandsteinsvöluberg: vel samt og heillegt. Grćnleitur. Sand- og siltboriđ. Nungr. Völur (grofa-möl). Heillt skeni á sprungur flötum. Sumastađar 3-4 mm fyllingar af hvitum og grćnl. Leir á skástigum spr. Fl.|Sandstone, sand and silt containing. Some precipitates. |Sediment|Sediment|Smectite-zeolite|2.88|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||3.5||
BUĐARHALS_55|58|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|189|Sandsteinsvöluberg: vel samt og heillegt. Grćnleitur. Sand- og siltboriđ. Nungr. Völur (grofa-möl). Heillt skeni á sprungur flötum. Sumastađar 3-4 mm fyllingar af hvitum og grćnl. Leir á skástigum spr. Fl.|Sandstone, sand and silt containing. Some precipitates. |Sediment|Sediment|Smectite-zeolite|2.88|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||3.5||
BUĐARHALS_56|59|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|193|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.85|Triple-weight|||0.16|Triple-weight||||||||||||||||||||||1.1||
BUĐARHALS_57|60|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|193|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.88|Triple-weight|||0.15|Triple-weight||||||||||||||||||||||0.7||
BUĐARHALS_58|61|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|193|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.90|Triple-weight|||0.18|Triple-weight||||||||||||||||||||||0.5||
BUĐARHALS_59|62|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.88|Triple-weight|||0.23|Triple-weight||||||||||||||||||||||0.6||
BUĐARHALS_60|63|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.88|Triple-weight|||0.18|Triple-weight||||||||||||||||||||||0.9||
BUĐARHALS_61|64|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|191|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.82|Triple-weight|||0.21|Triple-weight||||||||||||||||||||||0.9||
BUĐARHALS_62|65|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|191|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.75|Triple-weight|||0.18|Triple-weight||||||||||||||||||||||0.8||
BUĐARHALS_63|66|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Kargi: Rauđbrenndur og blöđróttur, samskonar og ađur. Leirfylltar sprungur (ţenjanlegur leir). Virđast út í ummyndađ basalt.|Scoria, flow-top breccia. Red and vesicular. Clay-filled cracks. Appear highly altered.|Lava flow|Flow-top breccia|Smectite-zeolite|2.88|Triple-weight|||0.21|Triple-weight||||||||||||||||||||||0.5||
BUĐARHALS_64|67|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||5.4||
BUĐARHALS_65|68|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple-weight|||0.08|Triple-weight||||||||||||||||||||||5.2||
BUĐARHALS_66|69|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|22.7.2000|Borehole|Búđarhálsvirkjun BH-9|483366|414119|-19.34275|64.22923|514|199|Basalt (olivínbasalt): Smákornótt ummyndađ basalt međ stuđlasprungum. Sumar stuđlasprungur eru fylltar at utfellingum. Skami af ţenjanlegum leira sprunguliđlum ser eru hrjúfir.|Altered Olivine Tholeiite: fine-grained altered basalt with columnar jointing. Some cracks are filled with secondary minerals. Some of the clay filled joint are rough-walled.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.94|Triple-weight|||0.09|Triple-weight||||||||||||||||||||||6.8||
BUĐARHALS_67|70|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|86|Basalt: ljósgrátt, fínkornótt. Smádilótt, plag. (2-4%). Ţétt en nokkrar smáblöđrur og finblöđruband. Fersk og óhlufyllt. Ljós leir og siltsteinn ó spr. Fl.|Tholeiite, light grey, small vesicles, rather fresh with some brown clay.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|3.09|Triple-weight|||0.05|Triple-weight||||||||||||||||||||||10.3||
BUĐARHALS_68|71|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|86|Basalt: ljósgrátt, fínkornótt. Smádilótt, plag. (2-4%). Ţétt en nokkrar smáblöđrur og finblöđruband. Fersk og óhlufyllt. Ljós leir og siltsteinn ó spr. Fl.|Tholeiite, light grey, small vesicles, rather fresh with some brown clay.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.99|Triple-weight|||0.05|Triple-weight||||||||||||||||||||||10.8||
BUĐARHALS_69|72|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|86|Basalt: ljósgrátt, fínkornótt. Smádilótt, plag. (2-4%). Ţétt en nokkrar smáblöđrur og finblöđruband. Fersk og óhlufyllt. Ljós leir og siltsteinn ó spr. Fl.|Tholeiite, light grey, small vesicles, rather fresh with some brown clay.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.99|Triple-weight|||0.06|Triple-weight||||||||||||||||||||||8.7||
BUĐARHALS_70|73|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|31|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.51|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||2.3||
BUĐARHALS_71|74|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|39|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.52|Triple-weight|||0.23|Triple-weight||||||||||||||||||||||3.1||
BUĐARHALS_72|75|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|39|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.56|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||1.6||
BUĐARHALS_73|76|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|39|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.54|Triple-weight|||0.22|Triple-weight||||||||||||||||||||||3.7||
BUĐARHALS_74|77|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|42|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.56|Triple-weight|||0.20|Triple-weight||||||||||||||||||||||2.2||
BUĐARHALS_75|78|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|42|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.53|Triple-weight|||0.28|Triple-weight||||||||||||||||||||||1.0||
BUĐARHALS_76|79|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.53|Triple-weight|||0.28|Triple-weight||||||||||||||||||||||1.6||
BUĐARHALS_77|80|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.54|Triple-weight|||0.29|Triple-weight||||||||||||||||||||||2.1||
BUĐARHALS_78|81|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.11.2000|Borehole|Búđarhálsvirkjun BH-12|482238|414714|-19.36607|64.23451|357|44|Samlímt liparít breksia. Pýrit fynnst á sprunguflötum. |Rhyolite (inhomogeneous), consolidated breccia, with pyrite in veins. |Silicic volcanic|Rhyolite breccia|Smectite-zeolite|2.51|Triple-weight|||0.26|Triple-weight||||||||||||||||||||||1.5||
BUĐARHALS_79|83|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.52|Triple-weight|||0.15|Triple-weight||||||||||||||||||||||4.5||
BUĐARHALS_80|84|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.54|Triple-weight|||0.16|Triple-weight||||||||||||||||||||||4.8||
BUĐARHALS_81|85|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.57|Triple-weight|||0.17|Triple-weight||||||||||||||||||||||3.9||
BUĐARHALS_82|86|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30|Liparit. Bergiđ er titlulega ferskt en ummyndađ á sprunguflötum. Straumflogott og smádilott af plagiokals. |Rhyolite (homogeneous), flow-banding, some alteration (brown and green)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.56|Triple-weight|||0.17|Triple-weight||||||||||||||||||||||4.4||
BUĐARHALS_83|88|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.90|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||1.9||
BUĐARHALS_84|89|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.73|Triple-weight|||0.15|Triple-weight||||||||||||||||||||||1.9||
BUĐARHALS_85|90|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.90|Triple-weight|||0.26|Triple-weight||||||||||||||||||||||2.2||
BUĐARHALS_86|91|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.90|Triple-weight|||0.24|Triple-weight||||||||||||||||||||||2.9||
BUĐARHALS_87|92|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.91|Triple-weight|||0.18|Triple-weight||||||||||||||||||||||1.6||
BUĐARHALS_88|93|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.89|Triple-weight|||0.23|Triple-weight||||||||||||||||||||||2.3||
BUĐARHALS_89|94|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|193|Sand-siltsteinn (ummyndađ): Hvarfleir-stöđuvatnasel. Logrétt lagskipt skiptast á greni sandst. Međ völum og illa samlimdur rauđi sillst. Liklega öll nokkuđ ummyndađ.|Sandstone, horizontal layering, mostly altered. |Sediment|Sediment|Smectite-zeolite|2.88|Triple-weight|||0.25|Triple-weight||||||||||||||||||||||2.9||
BUĐARHALS_90|95|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|14.8.2001|Borehole|Búđarhálsvirkjun BH-15|483036|414089|-19.34955|64.22894|515|193|Sand-siltsteinn (ummyndađ): Hvarfleir-stöđuvatnasel. Logrétt lagskipt skiptast á greni sandst. Međ völum og illa samlimdur rauđi sillst. Liklega öll nokkuđ ummyndađ.|Sandstone, horizontal layering, mostly altered. |Sediment|Sediment|Smectite-zeolite|2.83|Triple-weight|||0.23|Triple-weight||||||||||||||||||||||3.4||
BUĐARHALS_91|96|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|9.11.2000|Borehole|Búđarhálsvirkjun BH-11|482108|414828|-19.36876|64.23553|313|30||Rhyolite (homogeneous)|Silicic volcanic|Rhyolite lava|Smectite-zeolite|2.55|Triple-weight|||0.16|Triple-weight||||||||||||||||||||||4.2||
BUĐARHALS_92|97|Arngrímsson and Gunnarsson, 2009|Foged and Andreassen, 2016|28.8.2001|Borehole|Búđarhálsvirkjun BH-16|484359|413672|-19.32224|64.22526|430|108|VölubergŢ vel samlimt og brúnleitt. Grunnbariđ (sandur og silt). All lieslar völur nokkuđ nunar, mál, steinar og hnullungar. |Conglomerate, brown-colored, well-consolidated, sand and silt bearing.|Sediment|Sediment|Smectite-zeolite|2.94|Triple-weight|||0.27|Triple-weight||||||||||||||||||||||2.7||
Flovenz2005_2A|2A|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|16.6.1995|Borehole|Hengill ÖJ-1|390146|396973|-21.25010|64.07702|287|795|sjá borskýrsla Steingrímsson (1997) og fleiri rannsóknir hjá Franzson og Tulinius 1999|See drilling report in Steingrímsson (1997) and other studies in Franzson & Tulinius (1999)|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.59|Triple weight|||0.146|He gas pycnometry, Geological Survey of Denmark and Greenland|||||||352|0.0028373|0.002|0.0808|96.5||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_3|3 (KH-24)|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarđ|604229|577882|-16.73214|65.70167|606|172|Allt lagiđ er oxađ og blöđrur opnar og sumar fylltar. Sjá skýrslu Steingrímsson (1991). |Highly oxidized, with open vesicles, some of which are filled. See drilling report by Steingrímsson (1991). |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple weight|||0.022|Triple Weight|||||||||0.005|0.078|||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_3A|3A|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|24.2.1995|Borehole|Hengill ÖJ-1|390146|396973|-21.25010|64.07702|287|795|sjá borskýrsla Steingrímsson o.fl. 1997 og fleiri rannsóknir hjá Franzson og Tulinius 1999|See drilling report in Steingrímsson et al. (1997) and other studies in Franzson & Tulinius (1999),|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.46|Triple weight|||0.203|Scale and caliper|||||||303|0.0032992|2.90E-02|0.011166257|37.9||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||3.80|||||6.7|11.2|||
Flovenz2005_4|4|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|8.6.1995|Borehole|Nesjavellir NJ-17|388432|401653|-21.28864|64.11845|349|877|Borskýrsla Steingrimsson et al. (1994)|See drilling report in Steingrimsson et al. (1994)|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.80|Triple weight|||0.081|Triple Weight|||||||1177|0.0008495|4.01E-02|0.011193687|552||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_8|8|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|22.5.1995|Borehole|Reykjanes RN-8|319054|374424|-22.67676|63.87591|59|1005|Basalt túff|Basaltic tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.41|Triple weight|||0.199|Triple Weight|||||||||||90.6||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_9|9|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|27.5.1995|Borehole|Krafla KH-2, Sandabotnaskarđ|603109|578445|-16.75606|65.70045|543|166|Sjá borskýrslu Steingrímsson (1997)|See drilling report in Steingrímsson (1997).|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.71|Triple weight|||0.097|Triple Weight|||||||288|0.0034760|8.36E-02|0.011165204|227||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_11|11|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|24.6.1995|Borehole|Krafla KH-3, Sandabotnaskarđ|606657|580693|-16.67711|65.72609|760|402|Sjá borskýrslu Jónsson o.fl. 2003|See drilling report in Jónsson et al. (2003).|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.83|Triple weight|||0.022|Triple Weight|||||||||||||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_18|18|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|24.6.1995|Borehole|Krafla KH-3, Sandabotnaskarđ|606657|580693|-16.67711|65.72609|760|402|Sjá borskýrslu Jónsson o.fl. 2003|See drilling report in Jónsson et al. (2003).|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.80|Triple weight|||0.033|Triple Weight|||||||||||||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_47|47|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|25.6.1995|Surface|Heiđmörk |364980|398695|-21.76651|64.06478|148||Ferskt nútíma hraun sem hefur alldrei komizt niđur fyrir grunnvatnsborđ. Stađsetning ónákvćm|"Unaltered Holocene surface lava that has never been submerged below the groundwater
table. Location is very approximate. "|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.89|Triple weight|||0.083|Triple Weight|||||||1273|0.0007856|2.73E-03|0.048480005|100||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_58|58|Flóvenz et al., 2005|Kristinsdóttir et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarđ|604229|577882|-16.73214|65.70167|606|187|Smáblöđrusóna.  Sjá borskýrslu Steingrímsson (1997)|See drilling report in Steingrímsson (1997)|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.70|Triple weight|||0.105|Scale and caliper|||||||485|0.0020628|1.07E-01|0.014588439|450||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||3.80|||||13.0|11.2|||
Flovenz2005_61|61|Flóvenz et al., 2005|Kristinsdóttir et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarđ|604229|577882|-16.73214|65.70167|606|204|Sjá borskýrslu Steingrímsson (1997)|See drilling report in Steingrímsson (1997)|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.29|Triple weight|||0.192|Triple Weight|||||||31|0.0319337|6.42E-01|0.014040764|85||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Flovenz2005_71|71|Flóvenz et al., 2005|Kristinsdóttir et al., 2010|25.6.1995|Surface|Reykjanes peninsula|326867|381527|-22.52639|63.89396|56||Ferskt nútímahraun sem hefur aldrei fariđ niđur fyrir grunnvatnsborđ. Stađsetning ónákvćm. |"Unaltered Holocene surface lava that has never been submerged below the groundwater table. Location only very approximate.
table."|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.82|Triple weight|||0.117|Triple Weight|||||||1413|0.0007077|4.84E-03|0.01486217|72.6||Zahner IM-6 electrochemical workstation; measured over a range of frequencies|||||||||||
Nono2020_RN-17B|RN-17B|Nono et al., 2020|Reinsch et al., 2016|30.6.1995|Borehole|Reykjanes|318072|373574|-22.69566|63.86777|20|2802|RN17-B sýniđ er af grunnu sjávar gosbreksíu eđa móbergi í holu borađri 2008 in vinnsluholu RN17-B af 2801,6 m dýpi. Hátt ummyndunarstig innan amfíból beltis. Móbergiđ er misleitt fínkorna tekstúr og grunnmassa og blörđotta mola. . Ţađ er alummyndađ međ litla plagíóklasdíla, kalsít, sphen og aktínólít. XRD og EBSD analýsur  sýna fjórar steindir; plagíóklas, epidót, calsít og ágít. Plagíóklas smádílarnir eru andesín til albít. sjá IDDP-ICDP smákjarna í skýrslu Friđleifsson og Richter 2010.|RN17-B sample is a shallow marine volcanoclastic or hyaloclastic breccia drilled in 2008 in the production hole RN-17B at a depth of 2801.6 m. It shows a high degree of alteration in amphibolite facies. The hyaloclastite RN-17B displays a fine-grained inhomogenous texture and contains a groundmass and vesicular blasts. It is highly/pervasively altered and microcrysts of plagioclase, calcite, sphčne and actinolite. The XRD and electron backscattered diffraction image (EBSD) analyses show the presence of four major phases: plagioclase, epidote, calcite, and augite. Plagioclase microcrysts have composition from andesine to albite.See report about IDDP-ICDP spot Boreholes in Friđleifsson & Richter (2010).|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|3.00|Triple weight|||0.137|Triple Weight|9.88E-17|Same as air apparent permeability |||9.88E-17|Argon|1429|0.0007000|6.76E-03|0.0023|64|1.22|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|5.2|4.94|3.11|2.54|0.3||22.1|17.7|||
Nono2020_RN-19|RN-19|Nono et al., 2020|Reinsch et al., 2016|27.6.1995|Borehole|Reykjanes|319061|374147|-22.67629|63.87343|48|2246|Eins og fjallađ er um í skýrslu Friđleifsson o.fl. 2010, voru kjarnar borađir áriđ 2005 á 2238-2248 m dýpi. Sýni rannsakađ viđ UM ir af 2246 m dýpi. Sýniđ er úr dóleríti sem sýnir afar litla ummyndun. Og taliđ vera komiđ úr gangasveimi. Tekstúr er grófkorna og magmatískur. Sýniđ er fremur ferskt og sýnir engar gasblörđur. . dílarnir eru plagíóklas og klínó-pýroxen og er ţar ásamt klóríti, talki, oxíđi og kvartsi.  XRD og SEM/EBSD/EDS greiningar sýna tilveru ţriggja steinda; plagíóklas, ágít og klórít aog smávegis af talki, aktínólíti og kvars. plagíóklas sýnir ummyndunarsprungurmeđ anorthíti-andesíni. Klínópýroxeninn er af ágít samsetningu.  EBSD greining sýnir ađ ágítiđ og plagíóklas sýna óverulega kristalbyggingu eins og sýnt er á strerogrammi, sjá skýrslu IDDP-ICDP smákjarna  í Friđleifsson og RIchter 2010|As reported in Friđleifsson et al. (2010), RN-19 cores were drilled in 2005 at 2238 - 2248m depth. The sample investigated at UM is from a depth of 2246.2 m. This sample is a dolerite showing a relatively weak alteration and interpreted as a part of a sheeted dyke complex. The texture is coarse-grained and magmatic. The sample is relatively fresh and contains no apparent pores and veins. The phenocrysts are plagioclase and clinopyoxene and coexist with chlorite, talc, oxide and quartz. XRD and SEM/EBSD/EDS analyses show the presence of three major phases: plagioclase, augite and chlorite and few minor phases: talc, actinolite and quartz. Plagioclase show intergranular and intragranular cracks and a composition from anorthite to andesine. Clinopyoxenes have augite composition. EBSD analysis show that plagioclase and augite do not display significant crystallographic orientations, as shown on stereograms. See report about IDDP-ICDP spot Boreholes in Friđleifsson & Richter (2010).|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.75|Triple weight|||0.012|Triple Weight|1.32E-16|Same as air apparent permeability |||1.32E-16|Argon|5000|0.0002000|6.38E-04|0.00055|255.2567|2.32|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|3.8|5.70|2.36|2.49|0.4||13.9|17.1|||
Nono2020_RN-30|RN-30|Nono et al., 2020|Reinsch et al., 2016||Borehole|Reykjanes|318082|373572|-22.69545|63.86776|26|2519|Kjarnasýniđ kemur úr holu RN-30 af 2519 m dýpi. Bergiđ er mikródólerít međ plagíóklas, klínópýroxen, epidóti, kvars og oxíđ ásamr ráđandi klórít ummyndun. Textúr er óreglulegur og gerđur úr međalkorna magmatísku bergi. Kristallar eru mjög óreglulega sprungnir eins og velsést í ţunnsneiđum. magnummyndunarröđun (mest til minnst): palgíóklas, epidót, klínópýroxen, kvars. XRD greiningar sýna tilveru ágíts, plagíóklas og klóríts sem meginkristalla og minna af kvars og hornblendi sjá skýrslu  IDDP-ICDP smákjarnar Friđleifsson og RIchter. 2010|RN-30 sample comes from core drilled in the Reykjanes Peninsula at a depth of 2519 m. The sample is a microdolerite with plagioclases, clinopyroxene, epidote, quartz, and oxide and intensive chloritization. No orientation, foliation and pore system are observed. The texture is irregular/unregulated and is made of medium sized grains of magmatic origin. Minerals are intensively cracked and no crack orientations are observed on different thin sections. The order of alteration in mineral phases are (high to low): plagioclase, epidote, clinopyroxene, quartz. XRD analyses show the presence of augite, plagioclase and chlorite as major phases and quartz, hornblende as minor phases. The plagioclases have composition from bytownite to labradorite. Clinopyroxenes are augites. See report about IDDP-ICDP spot cores in Friđleifsson & Richter (2010).|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|3.02|Triple weight|||0.029|Triple Weight|2.39E-18|Same as air apparent permeability |||2.39E-18|Argon|3333|0.0003000|4.97E-03|0.0012|558.90395|2.37|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|4.6|5.65|2.60|2.63|0.4||17.0|20.8|||
Nono2020_NJ-17|NJ-17|Nono et al., 2020|Reinsch et al., 2016|8.6.1905|Borehole|Nesjavellir NJ-17|388432|401653|-21.28864|64.11845|340|877||NJ-17 sample was cored at a depth of 877m in the Nesjavellir - Hengill geothermal field. NJ-17 sample is a basaltic lava with porphyric texture of altered epidote and plagioclase set in a fine-grained, not orientated dark brown groundmass with prismatic-needles of plagioclase and microcrysts of oxides and clinopyroxene. XRD analyses indicate the presence of chlorite, quartz, calcite, and actinolite. Lava displays ellipsoidal/spherical to deformed pores. These small (50-100?m) pores are entirely filled with chlorite, whereas larger pores (up to 500?m) have chlorite rims and calcite and clinopyroxene, quartz or are empty. Few large phenocrysts, hypidiomorphic are highly altered: (1) long prismatic needles plagioclase (up to 500 ?m) or (2) tabular epidotes (cracked) and clinopyroxenes. In addition, the following observations have been made: - small veins are oriented N-S of thin-section, i.e. in direction of downhole, - cracks are not oriented, - lighter colored veins and dark brown/green cracks, - some rounded structures (former pores) are totally filled with orange-olive/brown mush including fine-grained epidote and clinopyroxene crystals, - possible orientation of light colored pores to the NE corner of the sample, - vesicle coalescence is observed, - irregular light colored veins connect pores with each other (filled with calcite and quartz), - where veins reach a pore, the dark brown mush chlorite-rims is often intersected/cut open. See core log in Steingrimsson et al. (1994).|Lava flow|Porphyritic basaltic lava|Chlorite-epidote|2.78|Triple weight|||0.180|Triple Weight|2.78E-17|Same as air apparent permeability |||2.78E-17|Argon|200|0.0050000|1.11E-01|0.00104|101.8012857|10.7|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|4.3|4.28|2.51|2.11|0.3||12.8|11.4|||
Nono2020_NJ-17B|NJ-17B|Nono et al., 2020|Reinsch et al., 2016|8.6.1905|Borehole|Nesjavellir NJ-17|388432|401653|-21.28864|64.11845|340|1009|KJarnasýni úr NJ17B af 100NJ-17B á 1009 m dýpi (132 m neđan NJ-17) á Nesjavöllum Hengli háhitakerfinu. NJ-17B er ummyndađ móberg, en er mjög klórít ríkt. Grunnmassinn er fínkorna aktínólít, klórít, plagíóklas og oxíđ. Stórar ílangar porur eru fylltar af klóríti viđ jađarinn og síđan kalsít, klínópýroxen og síđan oxíđ og plagíóklas í miđjunni. óreglulegar oxíđ ćđar eru til stađar, ásamt klórít ćđum. XRD griningar sýna fimm steindategundir. plagíóklas klórít, kalsít, aktínólít og ágít. Aktínólít hefur ekki fundist sem díll, og er líklegast ađ finna innan grunnmassans í tengslum viđ klórít. Sjá skýrslu Steingrimsson o.fl. (1994).|NJ-17B sample was cored at a depth of 1009 m (132 m below NJ-17) in the Nesjavellir - Hengill geothermal field. NJ-17B is an altered hyaloclastite (less than NJ-17), but with high degree of chloritization. The groundmass has fine-grained actinolite, chlorite, plagioclase, and oxides. Large elongated pores are filled with chlorite rims and calcite, clinopyroxene, and finally oxides and plagioclase in the pore centers. Irregular shaped oxide veins are present, extended by chlorite veins only. XRD analysis show the presence of five major phases of plagioclase, chlorite, calcite, actinolite, and augite. Actinolite has not been found as phenocrysts, and is probably included in the fine-grained groundmass in symbiosis with chlorite. See drilling report in Steingrimsson et al. (1994).|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.91|Triple weight|||0.121|Triple Weight|1.53E-18|Same as air apparent permeability |||1.53E-18|Argon|10|0.1010686|9.50E-03|0.101|138.5211429|11.9|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|4.5|4.56|2.67|2.29|0.3||15.7|14.2|||
IMAGE2016_ÖJ-1|ÖJ-1|Reinsch et al., 2016|||Borehole|Hengill ÖJ-1|390146|396973|-21.25010|64.07702|287|797|"Sýni úr kjarna í holul ÖJ-1 á Ölkelduhálsi af 797 m dýpi. Sýniđ er ummyndađ móbergstúff. Porur eru ađallega fylltar af klóríti. Ummyndunarútfellingar milli korna eru klórít, epidót, kvars, plagíóklas og kalsít, sum holými eru ekki fyllt. Rúnnuđ korn sem eru nokkurra milimetra breiđ međ dökku yfirborđi. stór fínkorna molar hafa dökk oxíđ, nanó-oxíđ/súlfíđ-nálar međ óreglulegri stefnu.  sum kornin hafa óreglulegar sprungur (nokkurra hundrađa microm og fáeina microm breiđar. sem fylltar eru kvarsi. stórir brúnir og grćnir (sjaldséđara) fínkorna hópar af ""xenomorphic"" prisma nálum međ nanó undirkonum úr epidóti og mögulega vaxiđ yfir af klóríti. XRD greiingar gefa víbendinga um sex kristalfasa: plagíóklas, klórít, kalsít, aktínólít, epidót og ágít."|ÖJ-1 sample was drilled in Ölkelduháls - Hengill area at a depth of 797m. ÖJ-1 sample is a hyaloclastitic tuff with hydrothermal texture. Pores and vesicles are mainly exclusively filled with chlorite. Interstitial fillings include chlorite, epidote, quartz, plagioclase and calcite. Sparse interstitial areas are not entirely filled with minerals (= holes). Rounded blasts have several mm-size large with darker rim. Large fine-grained blasts contain black oxides, nano-oxide/sulfide-needles that are unoriented. Few blasts have irregular-shaped cracks (several 100 ?m long and few ?m wide) filled with quartz. Large brown and greenish (less abundant) fine-grained mush of xenomorphic prismatic needles with nano-subgrains composed of epidote possibly overgrown by chlorite are present. XRD analyses indicate the presence of six major phases: plagioclase, chlorite, calcite, actinolite, epidote, augite.|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.86|Triple weight|||0.242|Triple Weight|1.29E-16|Same as air apparent permeability |||1.29E-16|Argon|||3.01E-03||31.7287|2.16|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|3.9|3.97|2.31|2.09|0.3||10.3|10.6|||
IMAGE2016_RW-17B|RW-17B|Reinsch et al., 2016|||Borehole|Reykjanes|318072|373574|-22.69566|63.86777|20|2804|RN-17B sýni er af móbergsbreksíu af grunnu sjávardýpi, tekiđ á 2804 m dýpi. Sýniđ er mjög ummyndađ í amfíból belti. Sýniđ er algerlega ummyndađ og međ blöđrótt og ţétt korn. Ríkt af fínkorna epidóti í plagíóklas og amfíól kristöllum. Porur sýna tengingu. Amfíból sést í fínkorna grunnmassa ásamt međ međalstórum blöđrum ţar sem epidót og plagíóklas fylla. sumar blöđrur eru tómar í miđju ţunnsneiđarinnar. XRD greiningar sýna ţrjá kristalfasa: plagíóklas, hornlendi og epidót. |RW-17B sample is a shallow marine volcanoclastic or hyaloclastic breccia drilled in 2008 in the production hole RN-17B at a depth of 2804m. It shows a high degree of alteration in amphibolite facies. This sample displays a pervasive hydrothermal alteration and contains vesicular and non-vesicular clasts. Intensive fine-grained epidote is present in a fine-grained plagioclase and amphibole matrix. The pore system is connected. Amphibole is present in a fine-grained matrix with medium-grained vesicle fillings of plagioclase and epidote. Some vesicles are empty in their center of thin section. XRD analyses exhibit the presence of three major phases: plagioclase, hornblende, and epidote.|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|2.99|Triple weight|||0.136|Triple Weight|4.34E-16|Same as air apparent permeability |||4.34E-16|Same as air apparent permeability |||4.36E-04||69.44883333|1.22|Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|4.8|4.61|2.99|2.41|0.3||21.3|16.0|||
IMAGE2016_GG1-porDol|GG1-porDol|Reinsch et al., 2016||14.5.2014|Surface|Geitafell|673425|441169|-15.39855|64.42795|213||Breksíerađ sýni tekiđ á mótum dílótts gabbró(dólerít) og umlykjandi basalts. Grćnleitar ummyndunarsteindir. |Brecciated sample taken at the contact between the porphyritic gabbro/dolerite and the host basalt. Infilling of secondary hydrothermal minerals of greenish color.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.84|Triple weight|||0.012|Triple Weight|||||||1038|0.0009630|7.80E-04|0.218622243|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG1-hrBa|GG1-hrBa|Reinsch et al., 2016|||Surface|Geitafell|673541|441052|-15.39628|64.42685|194||Ummyndađ basalt međ kvarsi/kalsíti (epidóti?) í ćđum.|Host rock: fine grained basalt; hydrothermal quartz/calcite (epidote?) forming a small vein and infilling cavities.|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.92|Triple weight|||0.008|He gas pycnometry||||||||||||||||||||||||
IMAGE2016_GG2-Dol|GG2-Dol|Reinsch et al., 2016|||Surface|Geitafell|673541|441052|-15.39628|64.42685|194||Dílalaust dólerít|Aphyric dolerite|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.66|Triple weight|||0.042|He gas pycnometry|1.62E-15|Same as air apparent permeability |||1.62E-15|Same as air apparent permeability |372|0.0026900|2.70E-03|0.0104|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG2-hrBa|GG2-hrBa|Reinsch et al., 2016|||Surface|Geitafell|673541|441052|-15.39628|64.42685|194||Basalt|Basalt|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.61|Triple weight|||0.079|He gas pycnometry|4.23E-15|Same as air apparent permeability |||4.23E-15|Same as air apparent permeability |173|0.0057700|5.67E-05|0.00593|833.3||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG3-Gab|GG3-Gab|Reinsch et al., 2016|||Surface|Geitafell|674925|443248|-15.36500|64.44580|791||Gabbró|Gabbro|Basaltic intrusion|Gabbro|Epidote-actinolite|2.89|Triple weight|||0.012|He gas pycnometry|||||||1279|0.0007820|9.10E-06|0.00448|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG4-GrPhy|GG4-GrPhy|Reinsch et al., 2016|||Surface|Geitafell|674925|443248|-15.39147|64.42452|116||Granófýr|Granophyre|Silicic intrusion|Granophyre|Chlorite-epidote|2.48|Triple weight|||0.028|He gas pycnometry|1.91E-15|Same as air apparent permeability |||1.91E-15|Same as air apparent permeability |234|0.0042800|4.32E-05|0.00462|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG4-porDol|GG4-porDol|Reinsch et al., 2016|||Surface|Geitafell|674925|443248|-15.39147|64.42452|116||Dílótt dólerít|Porphyritic dolerite|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.90|Triple weight|||0.009|He gas pycnometry|||||||422|0.0023700|2.41E-05|0.0104|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG7-porDol|GG7-porDol|Reinsch et al., 2016|||Surface|Geitafell|674177|440192|-15.38412|64.41882|81||D'ilótt dólerít|Porphyritic dolerite|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.95|Triple weight|||0.006|He gas pycnometry|||||||245|0.0040800|5.00E-07|0.0104|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GG7-hrBa|GG7-hrBa|Reinsch et al., 2016|||Surface|Geitafell|674177|440192|-15.38412|64.41882|81||Basalt|Basalt|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Triple weight|||0.006|Triple Weight|||||||840|0.0011900|1.10E-06|0.0104|||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_KH5-09|KH5-09|Reinsch et al., 2016|||Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|485|538|Gosbreksía|Volcanic breccia|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.12|Triple weight|||0.279|Triple Weight|9.64E-15|Same as air apparent permeability |||9.64E-15|Same as air apparent permeability |167|0.0060000|5.97E-05|0.00762|19.2||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_RN-17B|RN-17B|Reinsch et al., 2016|||Borehole|Reykjanes RN-17|318072|373574|-22.69566|63.86777|20||Misleit breksía međ móbergs grunnmassa. |Heterolithic breccia with hyaloclastite matrix|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|2.70|Triple weight|||0.136|Triple Weight|1.23E-15|Same as air apparent permeability |||1.23E-15|Same as air apparent permeability |222|0.0045100|4.10E-06|0.00593|58.1||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_RN-30|RN-30|Reinsch et al., 2016|||Borehole|Reykjanes RN-30|318082|373572|-22.69545|63.86776|26||Dólerít|Dolerite|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|2.92|Triple weight|||0.032|Triple Weight|||||||2058|0.0004860|4.90E-06|0.00593|434.8||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
IMAGE2016_GrPhy-L|GrPhy-L|Reinsch et al., 2016|||Surface|Reykjanes|||||||Granófýr|Granophyre|Silicic intrusion|Granophyre|Unaltered|2.45|Triple weight|||0.083|Triple Weight|1.08E-13|Same as air apparent permeability |||1.08E-13|Same as air apparent permeability |2681|0.0003730|2.50E-06|0.00549|35.6||Electrical conductivity measurements were conducted in the Paterson press at the Geosciences Laboratory of the University of Montpellier (France). This is an internally heated gas pressure vessel initially designed for high pressure (up to 500 MPa) and high temperature (up to 1300 °C) deformation experiments. Electrical conductivity was measured under dry and saturated conditions, applying a 2-poles configuration on cylindrical samples and using a Solartron 1260 impedancemeter.|||||||||||
Levy2018_02|L02|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|40|Sambrćdd breksía, Bergiđ er rauđleitara og aukning í fylltum sprungum. Mikiđ brotiđ og mjög ummyndađ. Rík a zeólítum  og pýríti, mjög ummynduđ. |Welded breccia; A lot of zeolites and pyrite, very altered|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.68|Triple weight|||0.360|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|3.26E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|2.47E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|3.26E-16|Argon|71|0.0141000|1.91E-01|1.30E-02|25|13.75| 2-poles, 1 kHz|2.9|3.14|1.67|1.45|||||||
Levy2018_05a|L05a|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|45|Mjög ummynduđ morkin breksía. Dćmigerđur HALARAUĐUR|Ignimbrite, very dense, low alteration level, iron rich|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.71|Triple weight|||0.215|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||237|0.0042200|1.27E-01|1.30E-02|113|7.33| 2-poles, 1 kHz|4.2|4.30|2.59|2.20|||||||
Levy2018_05b|L05b|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|45|Mjög ummynduđ morkin breksía. Dćmigerđur HALARAUĐUR|Ignimbrite, very dense, low alteration level, iron rich. Same as L05a but drilled in a different direction to analyze anisotropy.|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.72|Triple weight|||0.065|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|5.46E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||5.46E-19|Argon|||||474|7.33| 2-poles, 1 kHz|5.3|5.29|3.14|2.67|||||||
Levy2018_06|L06|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|49|Basaltbreksía međ rauđum molum í og hvítsett af útfellingu, sem eru í blöđrum.|Basalt breccia with oxidized grains and whitish deposition in vesicles|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.62|Triple weight|||0.264|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||7.50E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||65|0.0154000|4.10E-01|1.30E-02|75|30.88| 2-poles, 1 kHz|3.6|4.10|2.41|2.06|||||||
Levy2018_09|L09|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|60|Basaltbreksía. Mjög morkiđ, mikiđ um pýrít. 20 gr. Sprunga. Mjög morkiđ og brotiđ.|Basalt breccia, very crumbly abundant pyrite, heavily fractured|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.75|Triple weight|||0.275|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||33|0.0304000|1.02E+00|1.30E-02|89|36.42| 2-poles, 1 kHz|3.1|3.71|1.7|1.67|||||||
Levy2018_10|L10|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|66|Morkiđ fínk. Basalt|Crumbly fíne-grained basalt|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||0.302|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||80|0.0125000|3.77E-01|1.30E-02|71|23.16| 2-poles, 1 kHz|3.6|3.76|2.23|2.00|||||||
Levy2018_11|L11|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|69|Smáblöđrótt basalt. Straumflögótt, fínk. Basalt|FInely vesiculated basalt, flow lineated.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.90|Triple weight|||0.221|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|3.63E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|8.88E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|3.63E-17|Argon|68|0.0146000|7.66E-01|1.30E-02|186|21.95| 2-poles, 1 kHz|4.0|4.08|2.46|1.96|||||||
Levy2018_12a|L12a|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|70|Smáblöđrótt basalt. Straumflögótt, fínk. Basalt|FInely vesiculated basalt, flow lineated. HIghest density sample, with little alteration overall|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|3.04|Triple weight|||0.039|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||862|0.0011600|4.73E-02|1.30E-02|1005|5.07| 2-poles, 1 kHz|5.4|5.67|3.23|2.92|||||||
Levy2018_12b|L12b|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|70|Smáblöđrótt basalt. Straumflögótt, fínk. Basalt|Same as L12a but drilled in a different direction to study anisotropy.|Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|3.06|Triple weight|||0.047|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.23E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||1.23E-19|Argon|649|0.0015400|3.90E-02|1.30E-02|527|5.07| 2-poles, 1 kHz|5.5|5.76|3.17|2.93|||||||
Levy2018_14|L14|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|75|Morkiđ dökkgrátt túff|Hyaloclastite, crumbly and dark-grey|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.67|Triple weight|||0.395|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||2.57E-16|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||31|0.0325000|3.94E-01|1.30E-02|19|34.25| 2-poles, 1 kHz|2.7|2.89|1.49|1.26|||||||
Levy2018_15|L15|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|80|Bergiđ grátt og morkiđ. Stakar stórar blöđrur.|Grey crumbly rock, occasional large vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple weight|||0.105|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||131|0.0076300|2.37E-01|1.30E-02|267|17.17| 2-poles, 1 kHz|4.3|4.68|2.4|2.34|||||||
Levy2018_16|L16|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|99|Ljósgrćnt, ummyndađ og illa kristallađ.|Light green altered and partially crystallized|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.83|Triple weight|||0.098|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.09E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.48E-20|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.09E-17|Argon|102|0.0098400|3.12E-01|1.30E-02|293|19.88| 2-poles, 1 kHz|4.3|4.77|2.66|2.35|||||||
Levy2018_19|L19|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|120|Fínkornađ ţétt basalt|Dense fíne grained lava|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||0.216|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||3.16E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||118|0.0084700|2.82E-01|1.30E-02|122|20.65| 2-poles, 1 kHz|4.0|4.19|2.32|2.04|||||||
Levy2018_21|L21|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|126|Dökk sónasprunga - utf. Oxađ og ţétt|Dark fracture, oxidized and dense|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||0.149|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.09E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|9.28E-20|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.09E-17|Argon|90|0.0111000|4.07E-01|1.30E-02|211|25.09| 2-poles, 1 kHz|4.1|4.51|2.18|2.18|||||||
Levy2018_22|L22|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|131|Blóđrótt illa kr. Basalt|Vesicular, poorly crystalline lava|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.80|Triple weight|||0.139|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||7.90E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||27|0.0372000|1.24E+00|1.30E-02|207|23.16| 2-poles, 1 kHz|4.2|4.40|2.23|2.16|||||||
Levy2018_24a|L24a|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|144|Hólrými međ plötukalsíti o. fl. Mobergiđ er ţéttara hér.|Pore space filled with platy calcite. Hyaloclastite is thicker here. We found some organic carbon (maybe burnt tree root) in this sample.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.76|Triple weight|||0.222|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||26|0.0383000|9.56E-01|1.30E-02|88|28.46| 2-poles, 1 kHz|3.5|3.86|2.08|1.89|||||||
Levy2018_24b|L24b|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|144|Hólrými međ plötukalsíti o. fl. Mobergiđ er ţéttara hér.|Same as L24a but drilled in a different direction to study anisotropy.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.80|Triple weight|||0.178|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||29|0.0347000|1.22E+00|1.30E-02|163|28.46| 2-poles, 1 kHz|4.0|4.12|2.19|1.92|||||||
Levy2018_25|L25|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|151|Ljósgrá ummyndunarsóna. Sprunga - oxunarsteindir|Light grey alteration. Fractures. Some oxidized minerals. Extremely altered sample. Contains rare metals associated to pyrite (gold, platinum), it probably crosses an epithermal vein.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.81|Triple weight|||0.344|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.01E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|6.91E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.01E-17|Argon|23|0.0444000|8.55E-01|1.30E-02|37|12.78| 2-poles, 1 kHz|3.2|3.33|2.2|1.60|||||||
Levy2018_26|L26|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|158|Bergiđ betur kristallađ og er oxađ.|Rock better crystalized and oxidized|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.89|Triple weight|||0.099|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||145|0.0069000|1.50E-01|1.30E-02|200|14.23| 2-poles, 1 kHz|5.1|5.44|2.64|2.63|||||||
Levy2018_28|L28|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|167|Fínk. grátt ţétt basalt. Smá plag. dílar.|Fine grained dense basalt. Micro-plagioclase porphyritic|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.82|Triple weight|||0.136|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||169|0.0059300|6.87E-01|1.30E-02|740|33.77| 2-poles, 1 kHz|4.2|4.30|2.58|2.22|||||||
Levy2018_29|L29|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|174|Hraunlaga. Grátt. Oxađ berg og blöđrur yfirleitt opgnar.|Basalt lava, grey coloured. Oxidized rock with generally empty pores. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.84|Triple weight|||0.177|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||133|0.0075300|1.98E-01|1.30E-02|124|15.58| 2-poles, 1 kHz|4.5|4.94|2.66|2.42|||||||
Levy2018_30|L30|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|185|Gangberg. Smáblöđrur rađa sér í boga eins og um sprungu vćri ađ rćđa. |Dyke. Micro vesicles form a row |Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.85|Triple weight|||0.050|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||314|0.0031800|1.87E-01|1.30E-02|1125|11.34| 2-poles, 1 kHz|5.2|5.15|2.74|2.70|||||||
Levy2018_31|L31|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|189|Útfellingaríkt grćngrátt móbergstúff.|Extremely altered greyish green hyaloclastite tuff. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.77|Triple weight|||0.237|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||4.44E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||39|0.0258000|6.19E-01|1.30E-02|78|32.56| 2-poles, 1 kHz|3.6|3.62|1.92|1.46|||||||
Levy2018_35|L35|Levy et al., 2018|Jónsson et al., 2003|14.8.2002|Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|151|"Breksía, mest gerđ úr bergbrotum og međ ljósum ummynđuđum glergrunnmassa, mikiđ pýrít og kalsít. Breksían er mishörđ og međ ""stringers"" eđa ţunnum ţéttum basaltlögum. Orlítiđ finkornottari, annars sama bergiđ/myndunin."|Breccia, mostly of fractured rock and light coloured alteren groundmass. Pyrite and calcite rich. The breccia is variably hardened with stringers of tight thin basalt layers. |Lava flow|Flow-top breccia|Smectite-zeolite|2.61|Triple weight|||0.121|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||7.30E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||121|0.0082700|2.66E-01|1.30E-02|236|20.99| 2-poles, 1 kHz|4.5|4.67|2.73|2.18|||||||
Levy2018_36|L36|Levy et al., 2018|Jónsson et al., 2003|23.8.2002|Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|273|Breksía, engin. Almennileg lagskipting, vottur af graderingu, lau, an, cc, py.|Breksía. Layered, indication of gradation. Laumontít, ?, calcite and pyrite.|Lava flow|Flow-top breccia|Mixed-layer clay|2.81|Triple weight|||0.139|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||2.37E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||1164|0.0008590|1.82E-02|1.30E-02|146|3.14| 2-poles, 1 kHz|4.7|5.15|2.85|3.08|||||||
Levy2018_37|L37|Levy et al., 2018|Jónsson et al., 2003|24.8.2002|Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|325|Basalt, mjög blöđrótt og holufyllt, cc, qz, lau, heu. Ćđ eđa sprunga|Very vesiculated basalt with filled amygdales. Calcite, quartz, laumontite, heulandite.  Vein observed.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.75|Triple weight|||0.248|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||6.91E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||255|0.0039200|5.00E-02|1.30E-02|42|5.45| 2-poles, 1 kHz|3.7|4.27|2.41|2.03|||||||
Levy2018_40|L40|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|190|Ţétt kristallađ ljósleitt berg líklega basalt andesít/andesít, flókin bortatextúr međ nokkrar kynslóđir borta. Plötulaga kalsít og pýrít|Dense crystallized basalt or basalt andesite/andesite. Complex fracture systems with a few systems of different ages. Platy calcite and pyrite|Intermediate volcanic|Icelandite (andesite)|Mixed-layer clay|2.79|Triple weight|||0.234|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.46E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|3.36E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.46E-18|Argon|181|0.0055200|2.00E-01|1.30E-02|121|10.47| 2-poles, 1 kHz|4.0|3.85|2.33|2.11|||||||
Levy2018_41|L41|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|201|Kjarni víđ a brotin, misgengisbort međ slickenslides í 200,5 m, leir á brotfleti. Smásćtt KVARTS og leir í blöđrum|Core with number of fractures. Fault fractures with slickensides at 200,5 m. Clay in fracture. Small quartz and clay in vesicles. |Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.84|Triple weight|||0.113|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||289|0.0034600|5.23E-02|1.30E-02|122|4.1| 2-poles, 1 kHz|5.4|5.56|2.98|2.99|||||||
Levy2018_42|L42|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|226|Ljóst blöđrótt berg. WAIRAKÍT finnst gyrst í 224 m dýpi og finnst síđan viđ a í blöđrum međ kvartsi og eđa plötulaga kalsíti. Bergiđ er frauđkennt í 226 m dýpi en ţar kunna ađ vera lagamót. |Light coloured rock. Wairakite first found at 224 m depth and is widely found below in vesicles along with quartz and/or platy calcite. Rock is very vesicular in 226 m depth which may indicate a lava boundary. |Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.71|Triple weight|||0.306|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||189|0.0052900|8.53E-02|1.30E-02|39|6.75| 2-poles, 1 kHz|3.4|3.43|2.06|2.13|||||||
Levy2018_43|L43|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|268|Ljóst fínkorna blöđrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöđrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöđrum á 267 m dýpi. |Light coloured vesicular rock probably a lava of intermediate composition. Warakite in veins and vesicles along with quartz. Clays commonly found within many veins. Epidote found in vesicles at 267 m depth.|Intermediate volcanic|Icelandite (andesite)|Chlorite-epidote|3.03|Triple weight|||0.183|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1053|0.0009500|1.07E-02|1.30E-02|64|0.63| 2-poles, 1 kHz|4.7|4.84|2.89|2.23|||||||
Levy2018_44|L44|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|275|Ljóst fínkorna blöđrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöđrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöđrum á 267 m dýpi. |Light coloured vesicular rock probably a lava of intermediate composition. Warakite in veins and vesicles along with quartz. Clays commonly found within many veins. Epidote found in vesicles at 267 m depth.|Intermediate volcanic|Icelandite (andesite)|Chlorite-epidote|2.98|Triple weight|||0.214|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||592|0.0016900|2.08E-02|1.30E-02|53|0.92| 2-poles, 1 kHz|4.2|4.44|2.56|2.14|||||||
Levy2018_45|L45|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|277|Ljóst fínkorna blöđrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöđrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöđrum á 267 m dýpi. |Light coloured vesicular rock probably a lava of intermediate composition. Warakite in veins and vesicles along with quartz. Clays commonly found within many veins. Epidote found in vesicles at 267 m depth.|Intermediate volcanic|Icelandite (andesite)|Chlorite-epidote|2.93|Triple weight|||0.271|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||350|0.0028600|2.17E-02|1.30E-02|25|0.68| 2-poles, 1 kHz|3.5|3.69|2.08|1.86|||||||
Levy2018_46a|L46a|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|279|Ljóst fínkorna blöđrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöđrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöđrum á 267 m dýpi. |Light coloured vesicular rock probably a lava of intermediate composition. Warakite in veins and vesicles along with quartz. Clays commonly found within many veins. Epidote found in vesicles at 267 m depth.|Intermediate volcanic|Icelandite (andesite)|Chlorite-epidote|2.98|Triple weight|||0.244|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.99E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|4.93E-16|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|6.99E-16|Argon|725|0.0013800|8.26E-03|1.30E-02|28|0.43| 2-poles, 1 kHz|2.9|3.79|1.67|1.83|||||||
Levy2018_46b|L46b|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|279|Ljóst fínkorna blöđrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöđrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöđrum á 267 m dýpi. |Light coloured vesicular rock probably a lava of intermediate composition. Warakite in veins and vesicles along with quartz. Clays commonly found within many veins. Epidote found in vesicles at 267 m depth.|Intermediate volcanic|Icelandite (andesite)|Chlorite-epidote|3.01|Triple weight|||0.234|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||781|0.0012800|6.21E-03|1.30E-02|26|0.43| 2-poles, 1 kHz|3.0|3.87|1.52|1.77|||||||
Levy2018_47|L47|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|286|Dumbrauđleitt berg fínblöđrótt|Dark-red rock finely vesiculated|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.99|Triple weight|||0.240|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||433|0.0023100|1.77E-02|1.30E-02|30|0.34| 2-poles, 1 kHz|3.4|3.77|2.19|1.85|||||||
Levy2018_48|L48|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|288|Dumbrauđleitt berg fínblöđrótt|Dark-red rock finely vesiculated|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.96|Triple weight|||0.206|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||787|0.0012700|1.08E-02|1.30E-02|43|0.34| 2-poles, 1 kHz|4.1|4.18|2.32|2.25|||||||
Levy2018_49|L49|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|299|Grátt eđa ljósgrátt basalt - stórar wairakít holufyllingar, einnig stórir LAUMONTÍT kristallar|Grey and light grey basalt. Large wairakite vesicle fillings and large laumontite crystals|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|3.02|Triple weight|||0.103|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1949|0.0005130|6.52E-03|1.30E-02|136|0.19| 2-poles, 1 kHz|4.5|5.02|2.85|3.46|||||||
Levy2018_50|L50|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|303|Grátt eđa ljósgrátt basalt - stórar wairakít holufyllingar, einnig stórir LAUMONTÍT kristallar|Grey and light grey basalt. Large wairakite vesicle fillings and large laumontite crystals|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Triple weight|||0.232|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||1.58E-16|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||592|0.0016900|1.55E-02|1.30E-02|38|0.24| 2-poles, 1 kHz|4.2|4.18|2.37|1.99|||||||
Levy2018_51|L51|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|309|Grátt eđa ljósgrátt basalt - stórar wairakít holufyllingar, einnig stórir LAUMONTÍT kristallar|Grey and light grey basalt. Large wairakite vesicle fillings and large laumontite crystals|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.95|Triple weight|||0.281|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||524|0.0019100|2.03E-02|1.30E-02|34|0.77| 2-poles, 1 kHz|3.8|3.92|2.41|1.97|||||||
Levy2018_52|L52|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|323|Móbergsbreksíu|Hyaloclastite breccia   |Hyaloclastite|Pillow basalt|Mixed-layer clay|2.77|Triple weight|||0.144|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||260|0.0038500|8.37E-02|1.30E-02|133|5.11| 2-poles, 1 kHz|4.8|4.67|2.79|2.32|||||||
Levy2018_54|L54|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|346|Ţykk bólstrabergsmyndun, bólstrarnir eru međ rauđleitri slikju og sitja í grćnum velummynduđum grunnmassa. Ţessia myndun er frekar einsleit hefst í um 327 m dýpi og nćr niđur í um 364 m dýpi.|A thick pillow basalt formation. Pillows have reddish tint and are embedded in a well altered groundmass. This formation is rather homogeneous and starts at 327 m and extends down to 364 m depth|Hyaloclastite|Pillow basalt|Mixed-layer clay|2.80|Triple weight|||0.159|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1188|0.0008420|1.49E-02|1.30E-02|109|1.64| 2-poles, 1 kHz|4.5|4.63|2.39|2.68|||||||
Levy2018_55|L55|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|357|Ţykk bólstrabergsmyndun, bólstrarnir eru međ rauđleitri slikju og sitja í grćnum velummynduđum grunnmassa. Ţessia myndun er frekar einsleit hefst í um 327 m dýpi og nćr niđur í um 364 m dýpi.|A thick pillow basalt formation. Pillows have reddish tint and are embedded in a well altered groundmass. This formation is rather homogeneous and starts at 327 m and extends down to 364 m depth|Hyaloclastite|Pillow basalt|Mixed-layer clay|2.77|Triple weight|||0.160|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.84E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|9.87E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.84E-17|Argon|592|0.0016900|2.17E-02|1.30E-02|75|2.12| 2-poles, 1 kHz|3.9|4.50|2.33|2.35|||||||
Levy2018_56|L56|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|366|Ţykk bólstrabergsmyndun, bólstrarnir eru međ rauđleitri slikju og sitja í grćnum velummynduđum grunnmassa. Ţessia myndun er frekar einsleit hefst í um 327 m dýpi og nćr niđur í um 364 m dýpi.|A thick pillow basalt formation. Pillows have reddish tint and are embedded in a well altered groundmass. This formation is rather homogeneous and starts at 327 m and extends down to 364 m depth|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.72|Triple weight|||0.303|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||257|0.0038900|4.00E-02|1.30E-02|27|2.17| 2-poles, 1 kHz|3.7|3.74|2.21|1.89|||||||
Levy2018_57|L57|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|420|Settúff (eđa breksía) fer yfir í túff í um 402 m dýpi. Áberandi litlrikt túff, ummyndun bergsins almenntmíkil. |Sedimentary tuff (or breccia) that grades into primary tuff at about 402 m depth. Strikingly colourful tuff, and alteration generally high. |Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.88|Triple weight|||0.320|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.48E-15|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|6.91E-16|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.48E-15|Argon|226|0.0044200|2.92E-02|1.30E-02|17|1.16| 2-poles, 1 kHz|3.7|3.59|2.13|1.84|||||||
Levy2018_58|L58|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|429|Ljóst fínkorna ţétt basaltinnskot. |Light fine-grained dense intrusion|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.95|Triple weight|||0.127|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1017|0.0009830|4.45E-02|1.30E-02|326|3.38| 2-poles, 1 kHz|5.0|5.08|3.19|2.84|||||||
Levy2018_59|L59|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|430|Settúff (eđa breksía) fer yfir í túff í um 402 m dýpi. Áberandi litlrikt túff, ummyndun bergsins almenntmíkil. |Sedimentary tuff (or breccia) that grades into primary tuff at about 402 m depth. Strikingly colourful tuff, and alteration generally high. |Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.84|Triple weight|||0.220|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||306|0.0032700|5.43E-02|1.30E-02|63|3.81| 2-poles, 1 kHz|4.4|4.23|2.76|2.25|||||||
Levy2018_60|L60|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|464|Nokkur ţunn innskot eđa innskotsćđar í bólstrabreksíu.|A few thin basaltic intrusions or veins. Within a pillow breccia|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.85|Triple weight|||0.185|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||552|0.0018100|6.37E-02|1.30E-02|162|7.24| 2-poles, 1 kHz|4.4|4.38|2.6|2.47|||||||
Levy2018_61|L61|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|465|Móbergsbreksía, töluvert af bólstrabrotum efst í ţessari einingu en hlutfall bólstrabrota lćkkar er neđar dregur. |Hyaloclastite breccia, pillow fragments common in this unit but become more scarce in lower part. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.88|Triple weight|||0.347|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||243|0.0041200|2.37E-02|1.30E-02|14|2.75| 2-poles, 1 kHz|2.9|3.09|1.64|1.49|||||||
Levy2018_62|L62|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|512|Móbergsbreksía međ stórum ljósum bergrotum í miđhluta einingarinnar. |Hyaloclastite breccia with large basalt fragment within the central part of the unit. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.92|Triple weight|||0.185|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1543|0.0006480|1.41E-02|1.30E-02|116|0.77| 2-poles, 1 kHz|4.6|4.71|2.92|2.19|||||||
Levy2018_66|L66|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|546|Fersklegt basalt mjög ţétt efst en blöđróttara er neđar dregur, bólstramyndun (?)|Fresh basalt, compact at top but more vesicular downwards, possily a pillow basalt formation|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.92|Triple weight|||0.223|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1608|0.0006220|1.69E-02|1.30E-02|116|1.16| 2-poles, 1 kHz|4.4|4.44|2.55|2.33|||||||
Levy2018_67a|L67a|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|564|Breskía međ köntuđum litlum bergbrotum, ummyndunarsteindir eru epídót, kvarts, wairakít og kalsít ásamt leir|Breccia with angular basalt fragments. Alteraiton minaerals epidote, quartz, wairakite, calcite and clay.|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.84|Triple weight|||0.252|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||1230|0.0008130|1.02E-02|1.30E-02|53|0.43| 2-poles, 1 kHz|4.2|4.32|2.48|2.27|||||||
Levy2018_67b|L67b|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|564|Breskía međ köntuđum litlum bergbrotum, ummyndunarsteindir eru epídót, kvarts, wairakít og kalsít ásamt leir|Breccia with angular basalt fragments. Alteraiton minaerals epidote, quartz, wairakite, calcite and clay.|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.83|Triple weight|||0.274|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.40E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|7.90E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.40E-16|Argon|1000|0.0010000|9.44E-03|1.30E-02|38|0.43| 2-poles, 1 kHz|4.0|4.27|2.36|2.27|||||||
Levy2018_69|L69|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|495|Móbergsbreksía međ tltölulega ferskum basaltbrotum í garćnum vel ummynduđum grunnmassa|Basalt breccia containing relatively fresh basalt fragments embedded in grayish-green altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.93|Triple weight|||0.347|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|4.97E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.09E-16|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|4.97E-17|Argon|200|0.0050000|3.02E-02|1.30E-02|14|1.78| 2-poles, 1 kHz|3.6|3.49|2.29|1.79|||||||
Levy2018_71|L71|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|504|Móbergsbreksía međ tltölulega ferskum basaltbrotum í garćnum vel ummynduđum grunnmassa|Basalt breccia containing relatively fresh basalt fragments embedded in grayish-green altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.91|Triple weight|||0.371|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.07E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|5.72E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|6.07E-18|Argon|186|0.0053700|6.20E-02|1.30E-02|22|5.35| 2-poles, 1 kHz|3.7|3.50|2.28|1.94|||||||
Levy2018_73|L73|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|530|Ljósleitt smáblöđrótt berg, blöđrur liggja í taumum sem mynda 45 deg horn viđ borstefnu. Sprungur og sprugufyllingar eru nćr samsíđa blöđrutaumum|Light coloured finely vesiculated basalt. String like vesicle lines which form 45°angle to the direction of the drillhole.  Fractures and fracture fillings are near parallel to the string vesicles. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.99|Triple weight|||0.310|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||503|0.0019900|2.99E-02|1.30E-02|40|1.54| 2-poles, 1 kHz|3.8|3.80|2.36|2.20|||||||
Levy2018_75|L75|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|570|Móbergsbreksía međ tltölulega ferskum basaltbrotum í garćnum vel ummynduđum grunnmassa|Hyaloclastite breccia with relatively fresh basalt fragments embedded in heavily altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.91|Triple weight|||0.247|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||2041|0.0004900|1.45E-02|1.30E-02|117|0.63| 2-poles, 1 kHz|4.7|4.68|2.57|2.37|||||||
Levy2018_76|L76|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|573|Móbergsbreksía međ tltölulega ferskum basaltbrotum í garćnum vel ummynduđum grunnmassa|Hyaloclastite breccia with relatively fresh basalt fragments embedded in heavily altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.99|Triple weight|||0.099|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||2183|0.0004580|1.08E-02|1.30E-02|243|1.16| 2-poles, 1 kHz|5.1|5.23|2.79|3.29|||||||
Levy2018_77|L77|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|405|Ljósllitt berg međ óreglulegri blörudreifingu, hnígandi seig bráđ, hugsanlega gos undir jökli. Vaxkendur leir á lagmótum í 407 dýpi|Light coloured rock irregularly vesiculated, probably hyaloclastite. Soft clay at boundary at 407 m depth|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|||||0.160|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|5.68E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used||||||||||||4.4|5.10|2.64|2.81|||||||
Levy2018_80|L80|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|448|Syrpa af ljósu blöđróttu holufylltu basalti, bergiđ dökknar er neđar dregur. Á köflum er kjarninn mikiđ sprungin og viđa eru sprungufyllingar af kalsíti og kvartsi|Sequence of light coloured vesiculated basalt, rock becomes darker downwards. In places the rock is heavily fractured and calcite and quartz vein fillings common. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|||||0.107|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|5.68E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|2.66E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|5.68E-16|||||||||4.6|4.49|2.64|2.56|||||||
Levy2018_81|L81|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|461|Líklega örţunnt innskot í 460 m - Síđan mjög dökkt og fersklegt basalt frá 461 í 464,5 líklega innskot|Probably a thin basaltic intrusion at 460 m depth, than a very fresh and dark basalti from 461 to 464,5 m, probable intrusion. |Basaltic intrusion|Fine-medium grained basaltic intrusion|Mixed-layer clay|2.91|Triple weight|||0.080|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|3.48E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|9.87E-22|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|3.48E-18|Argon|198|0.0050500|2.02E-01|1.30E-02|461|20.26| 2-poles, 1 kHz|5.1|5.14|2.74|2.63|||||||
Levy2018_82|L82|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|487|Sprunga međ kvartsi og blađlaga kalsíti (qtz -> Cc -> qtz)|Basaltic lava very altered and argillized. Fracture with quartz and platy calcite.|Lava flow|Flow-top breccia|Mixed-layer clay|2.92|Triple weight|||0.342|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.92E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|6.51E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|6.92E-18|Argon|177|0.0056500|5.77E-02|1.30E-02|22|5.55| 2-poles, 1 kHz|4.3|4.11|2.52|2.60|||||||
Levy2018_85|L85|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|499|Glerjađ basalt. Hvítt WAIRAKÍT á eftir kvartsi í sprungufyllingu, einnig blađlaga kalsít|Basaltic lava poorly altered. Glassy basalt, wairakite following quartz in a vein filling, also platy calcite. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.93|Triple weight|||0.029|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.50E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.88E-21|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|6.50E-19|Argon|1004|0.0009960|1.96E-02|1.30E-02|683|3.86| 2-poles, 1 kHz|3.7|3.60|2.09|1.82|||||||
Levy2018_86|L86|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|501|Glerjađ basalt. Hvítt WAIRAKÍT á eftir kvartsi í sprungufyllingu, einnig blađlaga kalsít|Glassy basalt, wairakite following quartz in a vein filling, also platy calcite.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|||||0.076|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|4.33E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.68E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|4.33E-17|||||||||3.3|3.49|1.87|1.55|||||||
Levy2018_87|L87|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|509|Stórir laumontít kristallar í sprungufyllingu|Basaltic lava very altered and argillized. Large laumontite crystals in a fracture filling|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.91|Triple weight|||0.237|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.13E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||6.13E-18|Argon|629|0.0015900|5.47E-02|1.30E-02|119|5.4| 2-poles, 1 kHz|4.0|4.72|2.67|2.35|||||||
Levy2018_89|L89|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|515|Stórir laumontít kristallar í sprungufyllingu|Basaltic lava very altered and argilized, zone of fluid circulation. Large laumontite crystals in a fracture filling|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|||||0.113|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.82E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|8.49E-20|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.82E-19|||||||||3.2|3.42|2.19|1.73|||||||
Levy2018_91|L91|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|537|Stakdílótt bólstraberg|Sparsely plagioclase porphyritic pillow basalt.|Pillow basalt|Pillow basalt|Mixed-layer clay|2.86|Triple weight|||0.111|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.80E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|7.90E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.80E-18|Argon|877|0.0011400|6.41E-02|1.30E-02|462|8.1| 2-poles, 1 kHz|4.9|5.09|||||||||
Levy2018_93|L93|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|555|Fínkorna silti|Very fine-grained sill|Lava flow|Fine-medium grained basaltic intrusion|Unaltered|2.84|Triple weight|||0.240|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.51E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.68E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.51E-17|Argon|400|0.0025000|2.90E-02|1.30E-02|42|1.78| 2-poles, 1 kHz|3.4|1.64|3.11|1.45|||||||
Levy2018_95|L95|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|560|Breksía međ litlum oft rúnnuđum bólstrabrotum í grćnum grunnmassa, bólstrarnir eru ferskari en gunnmassin|Hyaloclastite breccia with round pillow fragments in a green matrix, pillows are fresher than the groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|||||0.244|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.37E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|5.92E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.37E-16|||||||||3.5|1.78|3.67|1.85|||||||
Levy2018_96|L96|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|582|Breksía međ litlum oft rúnnuđum bólstrabrotum í grćnum grunnmassa, bólstrarnir eru ferskari en gunnmassin|Hyaloclastite breccia with round pillow fragments in a green matrix, pillows are fresher than the groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.69|Triple weight|||0.279|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.17E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|5.92E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.17E-17|Argon|33|0.0305000|6.21E-01|1.30E-02|53|31.36| 2-poles, 1 kHz|3.3|1.77|3.31|1.54|||||||
Levy2018_97|L97|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|582|Breksía međ litlum oft rúnnuđum bólstrabrotum í grćnum grunnmassa, bólstrarnir eru ferskari en gunnmassin|Hyaloclastite breccia with round pillow fragments in a green matrix, pillows are fresher than the groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|||||0.251|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|4.02E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|8.88E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|4.02E-17|||||||||2.4|1.50|3.37|1.60|||||||
Levy2018_99|L99|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|587|Breksía međ litlum oft rúnnuđum bólstrabrotum í grćnum grunnmassa, bólstrarnir eru ferskari en gunnmassin|Hyaloclastite breccia with round pillow fragments in a green matrix, pillows are fresher than the groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.72|Triple weight|||0.305|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|5.11E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|5.53E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|5.11E-17|Argon|56|0.0177000|2.59E-01|1.30E-02|34|32.8| 2-poles, 1 kHz|4.3|2.57|4.37|2.35|||||||
Levy2018_100|L100|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|598|Breksía međ litlum oft rúnnuđum bólstrabrotum í grćnum grunnmassa, bólstrarnir eru ferskari en gunnmassin|Hyaloclastite breccia with round pillow fragments in a green matrix, pillows are fresher than the groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.80|Triple weight|||0.248|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.11E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|9.28E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.11E-17|Argon|197|0.0050700|2.41E-01|1.30E-02|147|0.96| 2-poles, 1 kHz|4.0|2.07|4.37|2.35|||||||
Levy2018_102|L102|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|623|Móbergbreksía međ rúnnuđum litlum bólstrabrotum, sem eru ljósgrá og frekar ferskleg, í grćnum ummynduđum grunnmassa|Hyaloclastite breccia with rounded small pillow fragments, which are light-grey and rather fresh, in green altered groundmass|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.69|Triple weight|||0.253|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|7.46E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.88E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|7.46E-17|Argon|127|0.0078900|1.00E-01|1.30E-02|39|9.84| 2-poles, 1 kHz|3.2|1.90|3.94|1.98|||||||
Levy2018_103|L103|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|707|Móbergbreskía sem fer yfir í bólstraberg í 699 m. Ţykk bólstrabergsmyndun, örlítiđ af grćnum millimassa milli bólstra.|Hyaloclastite on top of pillow rock at 699 m. Little bit of green groundmass between the pillows.  Sample taken from doleritic dyke moderately altered and argilized. |Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.96|Triple weight|||0.170|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.93E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||1.93E-18|Argon|901|0.0011100|3.98E-02|1.30E-02|187|5.93| 2-poles, 1 kHz|4.3|2.48|4.32|2.22|||||||
Levy2018_104|L104|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|724|Ţunnar innskotsćđar (eđa hugsanlega stór bólstri) í 724,5 m (40 cm ţykk) og í 735 m (30 cm ţykk) bergíđ er ţétt dökkt basalt.|Basaltic lava moderately altered and argillized. Thin intrusions or big pillows at 724.5 m|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.97|Triple weight|||0.124|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.70E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||1.70E-19|Argon|234|0.0042800|7.23E-01|1.78E-02|1194|21.78| 2-poles, 1 kHz|4.3|2.51|4.36|2.21|||||||
Levy2018_105|L105|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|727|Sammfelld móbergbreksía niđur í botn holunnar. Bólstrabrot eru frekar ferskeleg en millimassin er grćnn og vel ummyndađur. Í blöđrum bólstrabrotanna ber mest á kalsíti og kvarts|Hyaloclastite with basaltic mm to cm clasts of pillow basalt. Pillow fragments are fresher than groundmass which is green and altered. In the vesicles of the pillow fragments are calcite and quartz. |Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.75|Triple weight|||0.211|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|8.71E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|8.39E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|8.71E-17|Argon|46|0.0217000|3.69E-01|5.00E-02|66|24.85| 2-poles, 1 kHz|4.4|2.10|4.5|2.34|||||||
Levy2018_106|L106|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|298|Ţunnu hraunlagi|Thin basaltic lava |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Triple weight|||0.019|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.08E-20|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||1.08E-20|Argon|3846|0.0002600|1.91E-03|5.00E-02|578|1| 2-poles, 1 kHz|6.4|6.47|||||||||
Levy2018_107|L107|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|305|Basaltbreksía undir ţunnu hraunlagi međ LAUMONTÍTI, kalsíti og STILBÍTI|Basaltic breccia under thin lava layer with laumontite, calcite and stilbite.|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.82|Triple weight|||0.366|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|2.75E-16|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.18E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|2.75E-16|Argon|21|0.0468000|5.93E-01|5.00E-02|23|20.33| 2-poles, 1 kHz|3.3|2.98|||||||||
Levy2018_108|L108|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|338|Fínkorna dökktfersklegt basalt nćr blöđrulaust en mikiđ sprungiđ|Fine-grained, dark and fresh basalt with few vesicles but very fractured. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.86|Triple weight|||0.059|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|3.59E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||3.59E-19|Argon|645|0.0015500|4.77E-02|5.00E-02|521|9.95| 2-poles, 1 kHz|5.5|5.86|||||||||
Levy2018_109|L109|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|351|Syrpa af frekar fersklegu basalti (líklega hraunlög)|A series of rather fresh basalt (likely lava layers)|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.93|Triple weight|||0.043|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.63E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||1.63E-18|Argon|1059|0.0009440|1.52E-02|5.00E-02|411|7.2| 2-poles, 1 kHz|5.6|5.97|||||||||
Levy2018_110|L110|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|356|Syrpa af frekar fersklegu basalti (líklega hraunlög)|A series of rather fresh basalt (likely lava layers)|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.79|Triple weight|||0.154|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|4.35E-17|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.28E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|4.35E-17|Argon|37|0.0273000|4.27E-01|5.00E-02|88|9.12| 2-poles, 1 kHz|3.7|3.86|||||||||
Levy2018_111|L111|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|365|Syrpa af frekar fersklegu basalti (líklega hraunlög)|A series of rather fresh basalt (likely lava layers)|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.75|Triple weight|||0.051|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.22E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|8.78E-22|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.22E-18|Argon|358|0.0027900|1.01E-01|5.00E-02|693|6.82| 2-poles, 1 kHz|5.1|5.54|||||||||
Levy2018_112|L112|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|378|Smáblöđrótt basalt|Doleritic dyke moderately altered and argilized|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.85|Triple weight|||0.042|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|7.06E-20|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|||7.06E-20|Argon|893|0.0011200|3.71E-02|5.00E-02|803|6.14| 2-poles, 1 kHz|5.1|5.55|||||||||
Levy2018_113|L113|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|387|Smáblöđrótt basalt|Doleritic dyke very altered and argilized|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.92|Triple weight|||0.099|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|4.72E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|2.57E-21|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|4.72E-19|Argon|709|0.0014100|5.28E-02|5.00E-02|378|3.46| 2-poles, 1 kHz|4.9|5.29|||||||||
Levy2018_114|L114|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|394|Ljosara og frauđkenndara berg líklega ísurt|Doleritic dyke (possibly acidic) moderately altered and argilized|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.86|Triple weight|||0.073|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|6.17E-19|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|3.65E-21|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|6.17E-19|Argon|1100|0.0009090|2.81E-02|5.00E-02|445|2.54| 2-poles, 1 kHz|4.9|5.39|||||||||
Levy2018_115|L115|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b; Escobedo, 2018|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|403|Ljósleitt berg međ óreglulegri blöđrudreifingu, hnígandi seig bráđ, hugsanlega gos undir jökli. Vaxkendur leir á lagmótum í 407 m dýpi|Basaltic lava very altered and argilized|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.77|Triple weight|||0.148|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|1.18E-18|Measured with Argon gas and Klinkenberg corrected, steady-state flow, if permeability is less than 10^-19 pulse-decay is used|1.78E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|1.18E-18|Argon|216|0.0046400|1.35E-01|5.00E-02|178|5.98| 2-poles, 1 kHz|4.3|4.67|||||||||
Levy2018_116|L116|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|42|ţétt fremur fersklegt hraunlag, hópdílótt, vottur af oxun.|Compact fresh lava flow, porphyritic. Signs of oxidation|Lava flow|Porphyritic basaltic lava|Unaltered|2.94|Triple weight|||0.113|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||267|0.0037400|1.46E-01|5.00E-02|321|9.02| 2-poles, 1 kHz|4.9|5.19|||||||||
Levy2018_117|L117|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|48|ţétt fremur fersklegt hraunlag, hópdílótt, vottur af oxun.|Compact fresh lava flow, porphyritic. Signs of oxidation|Lava flow|Porphyritic basaltic lava|Unaltered|2.91|Triple weight|||0.051|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||337|0.0029700||5.00E-02||6.86| 2-poles, 1 kHz|5.7|5.98|||||||||
Levy2018_118|L118|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|54|ţétt fremur fersklegt hraunlag, hópdílótt, vottur af oxun.|Compact fresh lava flow, porphyritic. Signs of oxidation|Lava flow|Porphyritic basaltic lava|Unaltered|2.89|Triple weight|||0.049|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||348|0.0028700|1.03E-01|5.00E-02|716|6.88| 2-poles, 1 kHz|5.8|6.01|||||||||
Levy2018_119|L119|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|60|Móberg, mjög fínkorna og línt. Liturinn er grćnleitur og talsvert mikiđ af leir. Allar holur og holrými eru međ leir, py, cc. |Hyaloclastite, very fine grained. Green color, lot of clays. All the pore spaces are filled with clay, pyrite, calcite|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.59|Triple weight|||0.269|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||1.97E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||20|0.0499000|1.52E+00|5.00E-02|84|54.03| 2-poles, 1 kHz|2.6|3.29|||||||||
Levy2018_120|L120|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|71|Fremur grófkorna móbergstúff, kornin eru 4-10 mm. Ţessi myndun sem heldur áfram er fremur einsleitt.|Coarse grained hyaloclastite tuff. Grains of 4-10 mm size. Homogeneous formation.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.75|Triple weight|||0.390|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||3.75E-18|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||50|0.0201000|3.93E-01|5.00E-02|33|14.53| 2-poles, 1 kHz|3.1|2.91|||||||||
Levy2018_121|L121|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|73|Fremur grófkorna móbergstúff, kornin eru 4-10 mm. Ţessi myndun sem heldur áfram er fremur einsleitt.|Coarse grained hyaloclastite tuff. Grains of 4-10 mm size. Homogeneous formation.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.71|Triple weight|||0.401|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||6.42E-19|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||24|0.0414000|8.27E-01|5.00E-02|31|31.36| 2-poles, 1 kHz|2.8|2.73|||||||||
Levy2018_122|L122|Levy et al., 2018|Jónsson et al., 2003; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|83|Sama túffiđ, vćgar ásýndarbreytingar, kornastćrđ sveiflast til, og viđ eru linsur međ grófara efni, en allt sama túffiđ.|Same tuff as L120-121, with some changes. Lenses of coarser material, but overall same tuff.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.78|Triple weight|||0.387|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||2.17E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||36|0.0277000|3.91E-01|1.78E-02|23|24.9| 2-poles, 1 kHz|2.9|2.75|||||||||
Levy2018_123|L123|Levy et al., 2018|Gautason et al., 2007; Levy et al., 2019a,b||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|92|Gríđarlega mikiđ pýrít. Neđar verđur breyting og ţar tekur viđ fínkorna móbergstúff, mikill leir, mikiđ pýrít.|A lot of pyrite, lot of clay. Fine grained hyaloclastite.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.74|Triple weight|||0.365|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||2.07E-17|A servo-controlled pump with the pore pressure constant and the flow rate determined using measured piston displacemen|||10|0.1050000|1.78E+00|5.00E-02|30|35.22| 2-poles, 1 kHz|2.9|2.56|||||||||
Scott2022_200|L200|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|142.4|"Flott breksía, mest gerđ úr bergbrotum og međ ljósum ummynđuđum glergrunnmassa, mikiđ pýrít og kalsít. Breksían er mishörđ og međ ""stringers"" eđa ţunnum ţéttum basaltlögum. Orlítiđ finkornottari, annars sama bergiđ/myndunin."|"Breccia made of rock pieces, light colored alteration in the matrix, abundant pyrite and calcite. The breccia is heterogeneous with ""stringers"" or thin compact basalt layers. Slightly more fine-grained, otherwise the same lithology/alteration."|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.77|Triple weight|||0.310|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||13|0.0760543||6.80E-02||| 2-poles, 1 kHz|3.5|2.27|3.62|1.80|||||||
Scott2022_201|L201|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|153.5|Bólstrabrot eđa stór steinn. |Pillow piece or large fragment. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.70|Triple weight|||0.066|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||70|0.0141984||6.80E-02||| 2-poles, 1 kHz|4.6|2.78|4.64|2.44|||||||
Scott2022_202|L202|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|155.8|Merkileg skil í móberginu, hérna er komiđ í fínkorna túff, fín-lagskipt hálfgert set-túff og ummyndun minnkar. Túffiđ er dekkra og mun minna py. Fínkorna, leirkennt. Mjög einsleitt túff.|Fine grained tuff, alteration is reduced. Tuff is darker, less pyrite. Very homogeneous.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.71|Triple weight|||0.226|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||71|0.0140417||6.80E-02||| 2-poles, 1 kHz|5.3|2.99|5.42|2.65|||||||
Scott2022_203|L203|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|160.8|Basalttúff međ bergbrotum|Basaltic tuff with rock fragments. |Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.68|Triple weight|||0.340|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||60|0.0165938||6.80E-02||| 2-poles, 1 kHz|3.3|1.74|5.2|2.16|||||||
Scott2022_204|L204|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|169.2|Mjög einsleitt túff|Homogeneous tuff|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.57|Triple weight|||0.252|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||54|0.0184951||6.80E-02||| 2-poles, 1 kHz|3.2|1.45|3.86|1.69|||||||
Scott2022_205|L205|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|185.2|Steinar eđa stringers, í túffinu -- sem er ađ ţađ sama of ađ ofan.|Minerals or stringers in tuff, same as above.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.73|Triple weight|||0.246|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||203|0.0049208||6.80E-02||| 2-poles, 1 kHz|1.6|1.03|2.08|1.21|||||||
Scott2022_206|L206|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|192.4|Grćn leirdrulla, líklega millilag, eđa kargi.|Interlayer or flow-top breccia, green clay.|Lava flow|Flow-top breccia|Mixed-layer clay|2.75|Triple weight|||0.175|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||645|0.0015493||6.80E-02||| 2-poles, 1 kHz|5.6|3.15|5.72|2.86|||||||
Scott2022_207|L207|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|204.2|Fín-međalkorna basalt.|Fine-medium grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.93|Triple weight|||0.224|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||350|0.0028575||6.80E-02||| 2-poles, 1 kHz|2.4|1.24|2.31|1.59|||||||
Scott2022_208|L208|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|216.8|Mósaík-breksía.|Mosaic breccia|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.69|Triple weight|||0.258|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||61|0.0164407||6.80E-02||| 2-poles, 1 kHz|2.7|1.55|2.68|1.64|||||||
Scott2022_209|L209|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|234.7|Túff breksía, mikiđ af basalti|Tuff breccia, lot of basalt|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.55|Triple weight|||0.193|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||83|0.0120777||6.80E-02||| 2-poles, 1 kHz|2.6|1.49|2.62|1.51|||||||
Scott2022_210|L210|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|246.5|Mjög fínkorna túff, međ miklum perlitiskum textúr. Gjóskutúff, svolítiđ af bergbrotum.|Fine grained tuff, with perlite-like texture. Pyroclastic tuff with some rock fragments. |Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.21|Triple weight|||0.221|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||435|0.0022969||6.80E-02||| 2-poles, 1 kHz|2.9|1.75|3|1.66|||||||
Scott2022_211|L211|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|262.7|Móbergtúff, fínkorna međ talsvert miklu af bergbrotum.|Hyaloclastite tuff, fine grained with a lot of broken pieceS.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.57|Triple weight|||0.176|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||524|0.0019085||6.80E-02||| 2-poles, 1 kHz|3.8|2.25|3.47|2.27|||||||
Scott2022_212|L212|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|271.9|Breksía. Engin almennileg lagskipting, vottur af graderingu, lau, an cc, pyţ|Breccia. No clear layering, rather gradient. Laumontite, analcime, calcite, pyrite.|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.84|Triple weight|||0.199|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||292|0.0034254||6.80E-02||| 2-poles, 1 kHz|4.5|2.67|4.57|2.34|||||||
Scott2022_213|L213|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|318.7|Ljóst ţétt, sprungiđ og vöđlađ, gćti veriđ rhyólít, eđa ummyndađ brotaberg.|Light, compact, fractured. Could be rhyolite or altered broken rock|Silicic volcanic|Rhyolite breccia|Chlorite-epidote|2.69|Triple weight|||0.260|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||166|0.0060257||6.80E-02||| 2-poles, 1 kHz|4.9|2.65|5.41|2.46|||||||
Scott2022_214|L214|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|362.5|Breksía mikiđ laumontít.|Breccia with lot of laumontite|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.71|Triple weight|||0.147|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||746|0.0013401||6.80E-02||| 2-poles, 1 kHz|4.9|2.66|5.57|2.71|||||||
Scott2022_215|L215|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|377.8|Einsleitt basalt, bokkuđ blöđrótt beltar blöđrusónur, líklega hraunlagasyrpa.|Homogenous basalt, little alteration.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||0.055|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||624|0.0016035||6.80E-02||| 2-poles, 1 kHz|2.9|1.34|3.29|1.37|||||||
Scott2022_216|L216|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|152.4||BASALT, fresh, medium grey, small vesicles (<0.5cm), frequent phenocx: large plagio (<6mm), rare olivine+pyro|Lava flow|Porphyritic basaltic lava|Unaltered|2.94|Triple weight|||0.052|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||946|0.0010566||7.60E-02||| 2-poles, 1 kHz|3.9|2.24|4.4|2.03|||||||
Scott2022_217|L217|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|157.8||BASALT, dark grey, many large vesicles (<1.5cm), pheno cx: plagiodark grey, many large vesicles|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.95|Triple weight|||0.140|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||315|0.0031709||7.60E-02||| 2-poles, 1 kHz|4.7|2.76|4.79|2.91|||||||
Scott2022_218|L218|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|182.4||VOLCANIC SANDSTONE (TUFF), dark brown to black, unconsolidated in the upper part, well sorted, stratified|Hyaloclastite|Hyaloclastite sediment|Smectite-zeolite|2.82|Triple weight|||0.468|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||24|0.0412170||7.60E-02||| 2-poles, 1 kHz|5.4|3.05|5.53|3.17|||||||
Scott2022_219|L219|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|196.1||BASALT, fresh, fractured for the 1st top meter, fractures filled with angular clasts + greenish alteration (clay+chlorite?)|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple weight|||0.028|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||987|0.0010133||7.60E-02||| 2-poles, 1 kHz|5.6|3.15|5.72|2.86|||||||
Scott2022_222|L222|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|248.7||VOLCANIC BRECCIA, interbedded with BASALT showing flow structures, amygdules filled with Zeolite + reddish alteration|Lava flow|Hyaloclastite breccia|Smectite-zeolite|2.66|Triple weight|||0.482|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||20|0.0492320||7.60E-02||| 2-poles, 1 kHz|2.4|1.24|2.31|1.59|||||||
Scott2022_223|L223|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|260.4||VOLCANIC BRECCIA, dark brown to red (altered), with angular clasts up to 8cm, Zeolite filling, increasing in the size of the basaltic clasts up to 15cm downBorehole, vesicular basalt clasts filled with Zeolite and Quartz (?), some depth intervals are more altered, red, and clay rich|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.73|Triple weight|||0.469|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||32|0.0314030||7.60E-02||| 2-poles, 1 kHz|2.7|1.55|2.68|1.64|||||||
Scott2022_225|L225|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|302.7||VOLCANIC BRECCIA, dark brown to red (altered), with angular clasts up to 8cm, Zeolite filling, increasing in the size of the basaltic clasts up to 15cm downBorehole, vesicular basalt clasts filled with Zeolite and Quartz (?), some depth intervals are more altered, red, and clay rich; a little bit of chlorite but minimal, still smectite di|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.66|Triple weight|||0.396|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||13|0.0776253||7.60E-02||| 2-poles, 1 kHz|2.6|1.49|2.62|1.51|||||||
Scott2022_226|L226|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|312.7||VOLCANIC TUFF, clear grey, fine to coarse grained, probably of intermediate to acidic composition, fiame-like features (ignimbrite?), vertical to subvertical fracture in the lower part filled with white and soft mineralization (??) yugawaralite|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.40|Triple weight|||0.350|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||22|0.0449525||7.60E-02||| 2-poles, 1 kHz|2.9|1.75|3|1.66|||||||
Scott2022_227|L227|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|321.5||VOLCANIC BRECCIA, light grey to pinkish, well consolidated, poorly sorted, with large vesicular basalt clasts of several cm in size, vesicles filled with Zeolite (Scolecite/Mesolite?) and Quartz, amygdule  filled with Zeolite (Prehnite?) at around 329.4m depth; Alternating with TUFF layers of 1-2.5 m thick, Zeolite crystallization (Scolecite/Mesolite?) at a joint above 344 m depth, amygdule (2.5cm) filled with Quartz at about 350.8m depth, between 356.0 and 359.0m depth cm-size amygdules aligned along a 30cm old fissure and filled with Zeolite (Scolecite/Mesolite?), greenish clay (Chlorite?) within tuff matrix at about 354.5m depth|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.63|Triple weight|||0.303|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||84|0.0118431||7.60E-02||| 2-poles, 1 kHz|3.8|2.25|3.47|2.27|||||||
Scott2022_228|L228|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|334.4||VOLCANIC BRECCIA, light grey to pinkish, well consolidated, poorly sorted, with large vesicular basalt clasts of several cm in size, vesicles filled with Zeolite (Scolecite/Mesolite?) and Quartz, amygdule  filled with Zeolite (Prehnite?) at around 329.4m depth; Alternating with TUFF layers of 1-2.5 m thick, Zeolite crystallization (Scolecite/Mesolite?) at a joint above 344 m depth, amygdule (2.5cm) filled with Quartz at about 350.8m depth, between 356.0 and 359.0m depth cm-size amygdules aligned along a 30cm old fissure and filled with Zeolite (Scolecite/Mesolite?), greenish clay (Chlorite?) within tuff matrix at about 354.5m depth|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.83|Triple weight|||0.157|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||184|0.0054380||7.60E-02||| 2-poles, 1 kHz|4.5|2.67|4.57|2.34|||||||
Scott2022_229|L229|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|344.0||VOLCANIC BRECCIA, light grey to pinkish, well consolidated, poorly sorted, with large vesicular basalt clasts of several cm in size, vesicles filled with Zeolite (Scolecite/Mesolite?) and Quartz, amygdule filled with Zeolite (Prehnite?) at around 329.4m depth; Alternating with TUFF layers of 1-2.5 m thick, Zeolite crystallization (Scolecite/Mesolite?) at a joint above 344 m depth, amygdule (2.5cm) filled with Quartz at about 350.8m depth, between 356.0 and 359.0m depth cm-size amygdules aligned along a 30cm old fissure and filled with Zeolite (Scolecite/Mesolite?), greenish clay (Chlorite?) within tuff matrix at about 354.5m depth|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.89|Triple weight|||0.077|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||69|0.0144027||7.60E-02||| 2-poles, 1 kHz|4.9|2.65|5.41|2.46|||||||
Scott2022_230|L230|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|374.8||Succession of altered BASALT lava flows/lobes of 1-2m thick, dark grey, with their upper part vesicular and slightly oxidized, slight secondary mineralization of green Clay (Chlorite/Smectite?) in the non-vesicular and fine grained lower part, large white aureoles of alteration (fluid circulation) and red Clay alteration between 367 and 370m depth, cm-size amygdules filled with beautiful Zeolite fibers/crystals up to 1cm in size (e.g. Laumontite? between 385.5-388.5m, Yugawaralite? below 406.6m depth), reddish coloring downBorehole (Clay) with altered rock relatively easy to break by hand, narrow veins filled with white alteration due to fluid circulation|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.89|Triple weight|||0.047|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||110|0.0090574||7.60E-02||| 2-poles, 1 kHz|4.9|2.66|5.57|2.71|||||||
Scott2022_231|L231|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|429.4||Altered to very altered VOLCANIC BRECCIA and TUFF, dark grey to red in the upper part becoming light green in the lower especially between 428.7 and 442.5 cm depth, secondary mineralization of Chlorite/Smectite? almost entirely replacing the groundmass making it the rock fragile, the high degree of chloritization in addition to the more frequent occurence of Zeolite fibers of Laumontite type indicate temperature of the order of 200°C but less than 230°C as no epidote is observed|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|2.70|Triple weight|||0.258|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||50|0.0200085||7.60E-02||| 2-poles, 1 kHz|2.9|1.34|3.29|1.37|||||||
Scott2022_232|L232|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|444.1||Altered BASALT, light green to light gray, vesicular, vesicles filled with Quartz + Laumontite, Chlorite alteration less pronounced than in the overlying breccia|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.77|Triple weight|||0.165|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||150|0.0066615||7.60E-02||| 2-poles, 1 kHz|3.9|2.24|4.4|2.03|||||||
Scott2022_233|L233|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|450.8||Altered BASALT, light green to light gray, vesicular, vesicles filled with Quartz + Laumontite, Chlorite alteration less pronounced than in the overlying breccia|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.81|Triple weight|||0.145|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||275|0.0036372||7.60E-02||| 2-poles, 1 kHz|4.7|2.76|4.79|2.91|||||||
Scott2022_234|L234|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ŢR-07|594155|599552|-16.93578|65.89246|364|458.1||Altered BASALT, light green to light gray, vesicular, vesicles filled with Quartz + Laumontite, Chlorite alteration less pronounced than in the overlying breccia|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.77|Triple weight|||0.030|Plug mass was first measured on dry samples (dried at 60C in an oven for 48 hr), then measured on saturated samples, and finally measured in immersed conditions, saturated with low-salinity (about 100 ?S/cm), degassed water after evacuating air-filled pores in a vacuum chamber. University of Montpelier|||||||446|0.0022446||7.60E-02||| 2-poles, 1 kHz|5.4|3.05|5.53|3.17|||||||
Gilbert2020_P2-1|P2-1|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3648||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.01|Triple weight|||0.029|Triple weight|||||||2421|0.0004130|0.00039|0.063|322|||4.7|5.949|2.734|3.197|||||||
Gilbert2020_P2-2a|P2-2a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3648||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.04|Triple weight|||0.027|Triple weight|||||||1524|0.0006561|0.00074|0.063|330|||5.1|6.156|3.203|3.337|||||||
Gilbert2020_P2-2b|P2-2b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3648||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.04|Triple weight|||0.027|Triple weight|||||||1832|0.0005457|0.00035|0.063|235|||5.1|6.286|3.066|3.425|||||||
Gilbert2020_P2-3|P2-3|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3866||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.00|Triple weight|||0.022|Triple weight|||||||1321|0.0007568|0.00049|0.063|207|||4.8|5.961|2.778|3.419|||||||
Gilbert2020_P2-4|P2-4|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3856||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.00|Triple weight|||0.018|Triple weight|||||||1327|0.0007536|0.00038|0.063|218|||4.4|6.036|2.747|3.035|||||||
Gilbert2020_P2-5a|P2-5a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3869||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.02|Triple weight|||0.017|Triple weight|||||||1077|0.0009289|0.00055|0.063|159|||4.3|5.754|2.489|2.96|||||||
Gilbert2020_P2-5b|P2-5b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3869||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.02|Triple weight|||0.018|Triple weight|||||||1447|0.0006911|0.00043|0.063|195|||4.0|5.856|2.506|3.104|||||||
Gilbert2020_P2-6a|P2-6a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3869||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.01|Triple weight|||0.020|Triple weight|||||||1360|0.0007350|0.00056|0.063|188|||4.1|5.684|2.519|2.939|||||||
Gilbert2020_P2-6b|P2-6b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3869||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.02|Triple weight|||0.020|Triple weight|||||||1103|0.0009064|0.00085|0.063|201|||4.2|5.78|2.58|2.955|||||||
Gilbert2020_P2-7a|P2-7a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3870||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.01|Triple weight|||0.020|Triple weight|||||||1798|0.0005560|0.00038|0.063|223|||4.4|5.743|2.622|2.965|||||||
Gilbert2020_P2-7b|P2-7b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|3870||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.01|Triple weight|||0.022|Triple weight|||||||1325|0.0007547|0.00058|0.063|184|||4.6|5.804|2.759|3.229|||||||
Gilbert2020_P2-8|P2-8|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4090||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.03|Triple weight|||0.018|Triple weight|||||||846|0.0011819|0.00078|0.063|182||||5.245||2.577|||||||
Gilbert2020_P2-9|P2-9|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4255||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.04|Triple weight|||0.003|Triple weight|||||||8479|0.0001179|0.00015|0.063|640|||5.9|6.69|3.541|3.592|||||||
Gilbert2020_P2-10|P2-10|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4310||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.01|Triple weight|||0.009|Triple weight|||||||2167|0.0004614|0.00044|0.063|270|||4.6|5.965|2.841|3.102|||||||
Gilbert2020_PP1a|PP1a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4641||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.03|Triple weight|||0.027|Triple weight||||||||||||||2.4|4.617|1.486|2.146|||||||
Gilbert2020_PP1b|PP1b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4641||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.03|Triple weight|||0.025|Triple weight|||||||817|0.0012241|0.00015|0.063|64|||2.5||1.509||||||||
Gilbert2020_PP2a|PP2a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4649||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.05|Triple weight|||0.028|Triple weight|||||||872|0.0011467|0.00062|0.063|94|||2.3|4.69|1.51||||||||
Gilbert2020_PP2b|PP2b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4649||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.05|Triple weight|||0.029|Triple weight|||||||905|0.0011053|0.0003|0.063|92|||2.3|4.944|1.319|2.566|||||||
Gilbert2020_PP3a|PP3a|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4654||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.05|Triple weight|||0.017|Triple weight|||||||1319|0.0007583|0.00031|0.063|123|||4.2|5.505|2.569|3.046|||||||
Gilbert2020_PP3b|PP3b|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4654||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.05|Triple weight|||0.015|Triple weight|||||||1139|0.0008780|0.00052|0.063|162|||4.3|5.539|2.611|2.888|||||||
Gilbert2020_PP3c|PP3c|Gibert et al., 2020|||Borehole|Reykjanes IDDP-2|319001|374555|-22.67799|63.87706|66|4654||Dolerite from sheeted dike complex|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Epidote-actinolite|3.04|Triple weight|||0.015|Triple weight|||||||1474|0.0006783|0.00044|0.063|161|||4.6|5.652|2.838||||||||
Scott2020_Aust9X1 |Aust 9 X1 |This study|||Surface|Austurhorn gabbro|713029|442563|-14.57650|64.41790|220|||Layered oxide Gabbro with 70% plagioclase, 20% augite and 10% Fe-Ti oxides. Borehole parallel to lineation|Basaltic intrusion|Gabbro|Unaltered|2.89|Triple weight|||0.016|Triple weight|||||||893|0.0011200|0.001|0.09|200|||5.2|6.35|2.951|2.95|0.3||64.6|25.0|||
Scott2020_Aust9X1 |Aust 9 Y1 |This study|||Surface|Austurhorn gabbro|713029|442563|-14.57650|64.41790|220|||Layered oxide Gabbro with 70% plagioclase, 20% augite and 10% Fe-Ti oxides. Borehole perpendicular to lineation and in the foliation plane|Basaltic intrusion|Gabbro|Unaltered|2.89|Triple weight|||0.016|Triple weight|||||||709|0.0014100|0.0019|0.09|111|||4.4|6.18|2.439|2.75|0.3||43.5|17.1|||
Scott2020_Aust9Z1 |Aust 9 Z1 |This study|||Surface|Austurhorn gabbro|713029|442563|-14.57650|64.41790|220|||Layered oxide Gabbro with 70% plagioclase, 20% augite and 10% Fe-Ti oxides. Borehole perpendicular tofoliation plane|Basaltic intrusion|Gabbro|Unaltered|2.87|Triple weight|||0.018|Triple weight|||||||1144|0.0008740|0.0009|0.09|111|||5.5|6.40|2.735|2.83|0.3||55.8|21.3|||
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