|Reference||Sample information|||||||||Rock characterization|||||Grain density||Total porosity||Effective porosity||Permeability||||||Electrical properties|||||||Acoustic & mechanical properties|||||||
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|Lithology|Alteration zone|Grain density (g cm-3)|Remarks - grain density|Total porosity (%)|Remarks - total porosity|Effective porosity (%)|Remarks - effective porosity|Intrinsic permeability (m2)|Remarks - intrinsic permeability|Brine Apparent permeability (m2)|Remarks - Brine apparent permeability|Air Apparent permeability (m2)|Remarks - Air apparent permeability|Bulk resistivity (Ωm)|Bulk conductivity (S m-1)|Surface Conductivity (S m-1)|Fluid Conductivity (S m-1)|Formation Resistivity Factor (-)|Cation Exchange Capacity         (cmol+ kg-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)
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|Ummyndað set|Altered sediment|Sediment|Sediment|Altered|2.82|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Ummyndað þursaberg|Altered agglomerate|Hyaloclastite|Hyaloclastite breccia|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|22.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Ummyndað þursaberg|Altered agglomerate|Hyaloclastite|Hyaloclastite breccia|Altered|2.81|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-4|Pálsson et al., 1984|Pálsson et al., 1972|17.5.1969|Borehole|Ártúnshöfði 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-5|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1963|Borehole|Skyggnir við Elliðavatn 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-6|Pálsson et al., 1984|Pálsson et al., 1972|6.6.1963|Borehole|Skyggnir við Elliðavatn 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.7|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|16.3|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-9|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíðarbrekkur 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)|40.3|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|39.7|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-10|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíðarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|640|Fremur grófkristallað storkuberg með 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.3|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-11|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíðarbrekkur 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)|7.7|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.3|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-12|Pálsson et al., 1984|Pálsson et al., 1972|27.1.1967|Borehole|Hlíðarbrekkur Vestmannaeyjum H-1 (HB-1)|435940|327281|-20.28348|63.44490|95|1517|Basalt með 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)|5.3|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.3|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Ummyndað set|Altered sediment|Sediment|Sediment|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt 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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt 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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.04|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|36.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið 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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.03|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrótt 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)|20.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt basalt með 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|29.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Rauðleitt völuberg|Oxidized conglomerate|Sediment|Sediment|Unaltered|2.96|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|23.7|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|23.3|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|14.7|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-23|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerðishreppi H-1 (SH-1)|404420|382050|-20.94852|63.92876|20|35|Blöðrótt basalt, nokkuð 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-24|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerðishreppi H-1  (SH-1)|404420|382050|-20.94852|63.92876|20|58|Rauðleitt, blöðrulaust 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-25|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerðishreppi H-1  (SH-1)|404420|382050|-20.94852|63.92876|20|68|Blöðrulaust 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)|5.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-26|Pálsson et al., 1984|Pálsson et al., 1972|14.9.1967|Borehole|Sölvaholt í Hraungerðishreppi 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)|31.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með strjálum dálítið holufylltum blöðrum|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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Ummyndað 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Grænleitt, 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)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Ummyndað bólstraberg|Altered pillow lava|Hyaloclastite|Pillow basalt|Altered|2.93|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|15.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|12.3|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.7|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|19.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrótt, 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)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|22.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|20.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrótt, 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)|36.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|35.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-38|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 1|392508|393330|-21.19915|64.02639|102||Dökkgrænleitt túff með 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)|26.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|26.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-39|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 2|392508|393330|-21.19915|64.02639|102||Grænt túff|Green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|35.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|35.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-40|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-41|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 4|392508|393330|-21.19915|64.02639|102||Grænleitt túff með 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)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-42|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 5|392508|393330|-21.19915|64.02639|102||Súrt, straumlögótt gangberg með 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-43|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 6|392508|393330|-21.19915|64.02639|102||Grænleitt, ummyndað berg|Green-colored, altered rock|Hyaloclastite|Hyaloclastite tuff|Altered|2.76|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-44|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 7|392508|393330|-21.19915|64.02639|102||Ljósgrænt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|30.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-45|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 8|392508|393330|-21.19915|64.02639|102||Grænrauðleitt basalt með 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-46|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá 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)|2.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-47|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Grændalsá ofan Reykjakots í Ölfusi nr. 10|392508|393330|-21.19915|64.02639|102||Ljósgræntleitt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|21.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|19.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-48|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður A|393140|392391|-21.18559|64.01816|84||Grænleitt túff með 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-49|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður B|393140|392391|-21.18559|64.01816|84||Ljósgrænt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|31.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|30.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-50|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-51|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður D í sömu opnu og C, en 2 m neðar|393140|392391|-21.18559|64.01816|84||Grænleitt þursaberg|Green-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.75|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|11.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-52|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður E í 10 m lárétti fjarlægd frá D|393140|392391|-21.18559|64.01816|84||Grænbrúnt molaberg|Green-brown sedimentary rock|Sediment|Sediment|Unaltered|2.86|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|24.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-53|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Sauðá ofan Reykjakots í Ölfusi staður F|393140|392391|-21.18559|64.01816|84||Ljósgrænt túff|Light-green tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.77|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|23.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|22.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|34.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|26.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þétt, 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt, 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið, 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið, 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt, 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|31.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|25.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|23.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stakblöðrótt, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stakblöðrótt, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stakblöðrótt, 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|21.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|16.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|42.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|43.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-83|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 13|347971|384246|-22.09998|63.92823|290||Fíngert, grænleitt þursaberg|Fine, green-colored agglomeritic  breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|45.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|43.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|44.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|44.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-85|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 15|347971|384246|-22.09998|63.92823|290||Blöðrulítid, fínkornótt basalt með 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með 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)|25.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|23.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-87|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 17|347971|384246|-22.09998|63.92823|290||Blöðrulaust, 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|16.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|37.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|37.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|45.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|45.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 þursaberg|Red, fine-grained breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|50.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|49.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-91|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 21|347971|384246|-22.09998|63.92823|290||Ummyndað 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)||Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-92|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 22|347971|384246|-22.09998|63.92823|290||Rauðleitt túff|Oxidized tuff|Hyaloclastite|Hyaloclastite tuff|Altered|2.89|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|54.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|53.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-93|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 23|347971|384246|-22.09998|63.92823|290||Brúnleitt þursaberg|Brown-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.84|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|50.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|48.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-94|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sog á Reykjanesskaga nr. 24|347971|384246|-22.09998|63.92823|290||Fíngert, dökkbrúngrænleitt þursaberg|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)|49.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|49.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|51.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|49.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-96|Pálsson et al., 1984|Pálsson et al., 1972|4.5.1971|Borehole|Krísuvíkursvæði H-5 (KR-05)|351907|381525|-22.01720|63.90557|142|428|Ummyndað 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-97|Pálsson et al., 1984|Pálsson et al., 1972|4.5.1971|Borehole|Krísuvíkursvæði H-5 (KR-05)|351907|381525|-22.01720|63.90557|142|670|Ummyndað 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 stórblöðrótt, 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nærri blöðrulaust, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 smáblöðrótt, 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nærri blöðrulaust, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið, 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-107|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Hlíðarbrekkur Vestmannaeyjum H-1 (HB-1)|435941|327280|-20.28348|63.44490|95|782|Túffkennt þursaberg|Tuffaceous agglomerate|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.92|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|17.3|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.3|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Smáblöðrótt 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þursaberg|Agglomerate|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.00|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|31.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|28.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 að 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)|25.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|36.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|36.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|31.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|29.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|34.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|27.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|24.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 að 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)|31.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|30.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 að 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)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 að 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)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|35.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|28.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 að 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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|28.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|26.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nærri blöðrulaust, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt, 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|28.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nærri blöðrulaust, 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nærri blöðrulaust, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrótt, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Dálítið 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|27.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|26.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|26.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|24.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|24.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|25.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 með 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|23.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrótt, 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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|16.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|6.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Tæplega meðalblöðrótt, 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Stórblöðrótt, 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrulítið, 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|11.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Tæplega meðalblöðrótt, 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Blöðrulítið, 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt, 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)|11.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 smáblöðrótt, 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrótt, 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)|25.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 blöðrótt, 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|26.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Meðalblöðrótt, dílótt basalt, Tha eða 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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 smáblöðrótt, dílótt basalt, Tha eða 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-176|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 27|391294|393644|-21.22442|64.02882|189||Grænt túff með 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)|32.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|31.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-178|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 29|391294|393644|-21.22442|64.02882|189||Brúngrænleitt túff|Brown-green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.91|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|20.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-179|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 30|391294|393644|-21.22442|64.02882|189||Ljósgrátt, ummyndað berg|Light-gray altered rock|Hyaloclastite|Hyaloclastite tuff|Altered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|21.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-180|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 31|391294|393644|-21.22442|64.02882|189||Grágrænt, ummyndað 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)|20.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-182|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 33|391294|393644|-21.22442|64.02882|189||Ljósgrænt, ummyndað 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)|34.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|30.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-183|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 34|391294|393644|-21.22442|64.02882|189||Brúnleitt þursaberg|Brown-colored agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.81|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|38.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|36.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-184|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 35|391294|393644|-21.22442|64.02882|189||Ljósbrúngrænleitt túff|Light-brown-green tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.78|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|43.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|39.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-185|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Reykjadalur í Ölfusi nr. 36|391294|393644|-21.22442|64.02882|189||Blöðrulaust 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)|4.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|34.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-187|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Slaga í Sveifluhálsi á Reykjanesskaga|347589|378282|-22.10179|63.87463|283||Rautt þursaberg|Red agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.90|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|49.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|47.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-188|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvæði H-6|348640|386389|-22.08850|63.94772|145|412|Ummyndað 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-189|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvæði H-6|348640|386389|-22.08850|63.94772|145|413|Ummyndað 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-190|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvæði H-6|348640|386389|-22.08850|63.94772|145|625|Ummyndað 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-191|Pálsson et al., 1984|Pálsson et al., 1972|5.7.1971|Borehole|Krísuvíkursvæði H-6|348640|386389|-22.08850|63.94772|145|821|Ummyndað 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 þursaberg|Fine-grained breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|3.05|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|37.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|34.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-193|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Njarðvíkurheiði|327604|390687|-22.52179|63.97636|3|210|Dílalaust, blöðrótt 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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|16.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-194|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Njarðvíkurheiði|327604|390687|-22.52179|63.97636|3|497|Mjög fínkornótt, blöðrulaust 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-195|Pálsson et al., 1984|Pálsson et al., 1972|18.8.1971|Borehole|Krísuvíkursvæði H-7|348336|383153|-22.09147|63.91860|200|155|Blöðrulaust basalt með 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-196|Pálsson et al., 1984|Pálsson et al., 1972|18.8.1971|Borehole|Krísuvíkursvæði H-7|348336|383153|-22.09147|63.91860|200|186|Dílalaust, mjög blöðrulítið 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-197|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvæði H-8|349112|381938|-22.07447|63.90805|264|377|Brúnleitt, ummyndað 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-198|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvæði H-8|349112|381938|-22.07447|63.90805|264|378|Brúnleitt, ummyndað 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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-199|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvæði H-8|349112|381938|-22.07447|63.90805|264|736|Grænleitt berg með 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-200|Pálsson et al., 1984|Pálsson et al., 1972|26.10.1972|Borehole|Krísuvíkursvæði H-8|349112|381938|-22.07447|63.90805|264|930|Grænleitt berg|Green-colored rock|Hyaloclastite|Hyaloclastite tuff|Unaltered|3.01|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-203|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöðrótt basalt með 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)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-204|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Stórblöðrótt basalt með 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)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-205|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Misblöðrótt basalt með 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)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-206|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Smáblöðrótt 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)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-207|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöðrótt 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)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-208|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöðrótt, 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)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-209|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöðrulítið basalt með 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)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-210|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Blöðrulítið basalt með 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)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-211|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grindavík|||||||Stakblöðrótt basalt með 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)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-213|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niðri við sjó, IBF-4-810-5|||||||Grænt, hart túff með 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)|20.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|19.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-214|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niðri við sjó, IBF-4-810-6|||||||Grænt, hart túff með 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)|23.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-215|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kléberg á Kjalarnesi niðri við sjó, IBF-4-810-7|||||||Grænt, hart túff með 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)|21.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|19.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-216|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Leiðhamar við Kollafjörð undir Háspennulínu, IBF-4-810-8|||||||Grænt, hart túff með 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)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-217|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan við Ártún, IBF-2-137-2|||||||Dílótt þóleiít 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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-218|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Lokufjall, IBF-2-197-1|||||||Þóleiít 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)|1.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-219|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Lokufjall við Tíðaskarð, 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-220|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestanvert Kerlingagil, IBF-1-166-1|||||||Dílótt þóleiít 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-221|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, suðvestan Tindstaðahnúkur, IBF-1-46-5|||||||Þóleiít 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-222|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, áin austan við bæinn Flekkudal, IBF-1-97-3|||||||Þóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-223|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestan við Kerhólakamb, IBF-2-28-1|||||||Dílótt þóleiít 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-224|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vestan í Skálatindi, IBF-1-246-1|||||||Fínkornótt ólvivínþóleiít 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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-225|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, vesturhlíð Eilísfdals, IBF-1-226-1|||||||Fínkornótt ólvivínþóleiít 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-226|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norðan í þórnýjartindi, IBF-1-216-3|||||||Ólivínþóleiít 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-227|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Þverárdalur, IBF-1-99-1|||||||Þóleiít 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-229|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norðan við Leirvogsá, suðvestan Tröllafoss, IBF-259-7|||||||Þóleiítdólerít úr stuðluðu 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-230|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sunnan í stardalshnúk, IBF-249-4|||||||Ólivínþóleiítdólerít úr stuðli|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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-231|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norðan í þórnýjartindi, IBF-1-216-2|||||||Fínkornótt þóleiít 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)|10.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-232|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Múli, IBF-1-229-6|||||||Líparít, blöðrur að 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-234|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, í gili sunnan við 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-235|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan í Kistufelli, IBF-1-128-1|||||||Dílótt þóleiít|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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-236|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grímmannsfell, Austan í Dalhólum, IBF-2-228-2|||||||Fínkornótt ólivínþóleiít 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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-237|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Við Leirvogsá, vestan við 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)|22.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|19.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-238|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Kerlinagil, IBF-4-2611-1|||||||Þóleiít úr miðju 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-240|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Kerlinagil, IBF-4-2611-3|||||||Þóleiít úr miðju 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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-244|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Melafjall, IBF-4-46-9|||||||Blöðrótt, straumlögótt þóleiít|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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-245|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norðurhlíð Melafjalls, IBF-4-46-10|||||||Ólivínþóleiít|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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-246|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, sunnan Tíðaskarðs, við mynni Blikdals, IBF-4-46-12|||||||Ólívínþóleiít|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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-247|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sunnan Tindstaða. IBF-1-296-1|||||||Dílótt þóleiít 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-248|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norðurhlíð Sneiða, IBF-5-204-2|||||||Stórdílótt þóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-249|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Sneiðar, IBF-5-204-1|||||||Dílótt ólivínþóleiít 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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-250|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, suðvestan við Kerhólakamb, IBF-2-28-1|||||||Dílótt þóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-251|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, norðaustan í þórnýjartindi, IBF-1-216-1|||||||Dílótt ólívínþóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-252|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Þverárkotsháls, IBF-39-1|||||||Dílótt ólivínþóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-253|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, Nónbunga, IBF-1-87-1|||||||Ólivínþóleiít 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)|15.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-254|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norðan við Helgafell í Mosfellssveit, IBF-1-259-7|||||||Þóleiít 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-255|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Esja, austurhlíð Trönu, IBF-1-37-2|||||||Dílótt þóleiít 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)|8.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|1.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Nær eingöngu basalt, þursaberg|Agglomeritic breccia|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.85|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-258|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur við Hjörleifshöfða|324217|511259|-18.77461|63.42308|19||Þursaberg|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)|23.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-259|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur við Hjörleifshöfða|324217|511259|-18.77461|63.42308|19||Gjallkennt basalt eða 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)|37.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-260|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kötluklettur við Hjörleifshöfða|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)|35.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-264|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Geldingsadalsfjall í Gnúpverjahreppi|394901|438355|-20.26216|64.05173|107||Blöðrótt, nokkuð 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)|24.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-265|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll|458923|488525|-19.23995|64.63134|1162||Blöðrótt 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)|22.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-266|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|386600|496920|-19.06290|63.98277|669||Blöðrótt 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-267|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|386600|496920|-19.06290|63.98277|669||Líparít úr miðjum 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)|23.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|26.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-270|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár við 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|17.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-272|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll, Fremri-Árskarðsá|458923|488525|-19.23995|64.63134|1162||Basaltandesít úr miðjum 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)|29.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-273|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kerlingarfjöll, Norðausturhlíð Loðmundar|458923|488525|-19.23995|64.63134|1162||Mjög blöðrótt andesít, 99.9% syrtið (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)|42.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|35.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-276|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Selfjall suðvestan 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)|4.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|57.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|53.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-278|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Brimnes Norðan Kollafjarðar, IBF-5-3010-1|||||||Dílótt þóleiít 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|6.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|6.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-281|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Kálfstindar|||||||Blöðrótt, 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)|35.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|29.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 ummyndað þursaberg|Tuffaceous very altered agglomerate breccia|Hyaloclastite|Hyaloclastite breccia|Altered|2.70|Measured on crushed sample, pycnometry, column rho_2 in Pálsson et al. (1984)|15.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þétt 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)|4.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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, blöðrulítið 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)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-289|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-1 (FV-1)|686755|506955|-15.03688|65.06161|603|101|Blöðrulítið 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)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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, blöðrulaust 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)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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, blöðrulítið 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)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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, blöðrulítið 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)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-293|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|39|Rauðbrúnt, fínkornótt þursaberg|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)|24.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-294|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|39|Rauðbrúnn 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)|21.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-295|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-2 (FV-2)|686338|507831|-15.04454|65.06970|626|142|Stórblöðrótt, 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)|20.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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, böðrulaust 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)|2.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-297|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Fljótsdalur FS-3 (FV-3)|686051|508455|-15.04979|65.07546|640|14| Blöðrulítid, 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)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-298|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Mjóifjörður við Ísafjarðardjúp|603169|338429|-22.54422|65.88470|139||Stakblöðrótt 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)|0.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-299|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Ísafjörður|625860|314147|-23.10776|66.07464|5||Smádílótt, nærri blöðrulaust 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)|0.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-300|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Skötufjörður|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)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-301|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Álftafjörður við Ísafjarðardjúp|615922|317512|-23.01966|65.98764|12||Gráleitt basalt með fáum holufylltum blöðrum|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)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-302|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Hestfjörður|613111|324581|-22.86056|65.96643|82||Grátt, dílótt, blörulítið 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)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-303|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Norðvesturhlíð Bláhnúks (Laugahnúks) við Landmannalaugar|386645|496333|-19.07489|63.98317|673||Blöðrulítið líparít úr gangi eða 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|12.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-304|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíð Bláhnúks (Laugahnúks) við Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miðjum 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-305|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíð Bláhnúks (Laugahnúks) við Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miðjum 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|15.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-306|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíð Bláhnúks (Laugahnúks) við 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)|7.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-307|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) við 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)|26.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|23.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-308|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) við 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)|33.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|32.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-309|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) við 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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-310|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-311|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-312|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|386600|496920|-19.06290|63.98277|669||Líparít úr miðjum 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-313|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) við 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)|30.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|27.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-314|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stapafell|||||||Basalt úr miðjum 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|16.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|34.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|23.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-316|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stapafell|||||||Basalt neðarlega 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)|26.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-317|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Bláhnúkur (Laugahnúkur) við Landmannalaugar|386645|496333|-19.07489|63.98317|673||Líparít úr miðjum 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)|23.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|18.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-318|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Vesturhlíð Bláhnúks (Laugahnúks) við 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-319|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöðrótt 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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-320|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöðrulaus 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)|9.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|3.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-321|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöðrótt, 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)|28.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|17.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-322|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar|388410|497183|-19.05756|63.99901|663||Blöðrótt, 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-323|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|386600|496920|-19.06290|63.98277|669||Blöðrulaus 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)|2.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|1.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-324|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Landmannalaugar, Grænagil|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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|14.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-325|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Stuðlað 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)|21.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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 miðjum 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-327|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár við Brúna|407518|493284|-19.13810|64.17036|432||Basalt úr miðjum 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)|11.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|5.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-331|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sigalda Sunnan Tungnár við Brúna|407518|493284|-19.13810|64.17036|432||Basalt úr miðjum 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)|14.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|12.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-333|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Líparít úr miðjum 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|3.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|5.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|0.1|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-337|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Líparít úr miðjum 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)|16.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-338|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Stuðlað 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)|19.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|13.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-339|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Stóragil vestan í strút|446405|670077|-15.46185|64.47654|610||Blöðrótt 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)|13.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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)|18.0|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|16.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
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|Þétt ólivínþóleiít|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)|3.5|Calculated after measuring grain density on pulverized sample, phi_tot = 1 - (rho_dry/rho_grain); named phi_2 in Pálsson et al. (1984)|4.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-342|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Grenivík|606155|537223|-18.18183|65.94994|3||Dökkt, ólivíndílótt, stakblöðrótt 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)|||2.5|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-343|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Helguvík á Rosmhvalanesi B-9|||||||Fínblöðrótt 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)|||8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-344|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Helguvík á Rosmhvalanesi B-10||||||18|Stórblöðrótt 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)|||19.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-345|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarðvík|||||||Blöðrulítið 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)|||9.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-346|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarðvík|||||||Fremur blöðrulítið 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)|||7.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-347|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Njarðvík|||||||Mjög blöðrulítið 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)|||11.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-348|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Keflavík|||||||Mjög blöðrulítið 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)|||10.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-349|Pálsson et al., 1984|Pálsson et al., 1972||Surface|Sandgerði|||||||Mjög blöðrulítið 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)|||8.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
P-350|Pálsson et al., 1984|Pálsson et al., 1972||Borehole|Laugardælir ÞG-12 ||||||305|Rautt túff|Red oxidized tuff|Hyaloclastite|Hyaloclastite tuff|Unaltered|||||45.0|Measured after weighing sample in dry, saturated and immersed conditions, calculated as phi_eff = (rho_sat - rho_dry)/(rho_sat - rho_immersed)|||||||||||||||||||||
G-1|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440824|-15.39058|64.42466|132||Súr gangur úr fasa 4 og æðakerfi 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|6.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.2|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|||||||||||||||
G-2|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440828|-15.39059|64.42469|133||Breksía 3 m austan við sýni G-1, þ.e. mjög sprungin basalt breksía og sprungur fylltar. Sýni tekið 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|7.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|7.1|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|||||||||||||||
G-3|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673829|440845|-15.39056|64.42484|136||Fínkornótt þóleiítbasalt hraunlag. M.a. epidót, klórít og prenít í blöðrum. Bergid er blöðrótt, en fyllt og mjög þétt 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|3.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-4|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673793|440982|-15.39115|64.42609|155||Plagíóklasporfýr með þéttum grunnmassa. Allar blöðrur 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|4.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-5|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673792|440988|-15.39115|64.42614|156||Plagíóklasporfýr. Blöðróttur með morkna ásýnd, blöðrur fylltar að hálfu eða öllu leyti. Berg mjög brotið og straumflögótt. Sýni tekið við neðri jaðar 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|19.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|19.4|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|||||||||||||||
G-6|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673793|440997|-15.39112|64.42623|159||Sama lag og G-5 en í þéttara bergi líklega 6 m ofar. Bergið er plagíóklas- dílótt, með þéttum grunnmassa annars á lýsingin við 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|5.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-7|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|673797|441009|-15.39103|64.42633|162||Enn sama berg en nú 1-2 m ofan við G-6 og 1 m neðan við keilugang. Bergið er plagíóklas-dílótt, með þéttum grunnmassa annars á lýsingin við 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|5.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-8|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674155|441306|-15.38326|64.42880|199||Plagíóklasdílótt straumflögótt basalthraunlag með fínkornóttum þéttum millimassa. Sýnið tekið úr blöðróttum neðri hluta lagsins. Ljósgrænn leir fyllir blöðrur, zeólítar (m.a. skólesít og laumontít) og epidótæðar 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|17.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.1|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|||||||||||||||
G-9|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674156|441310|-15.38323|64.42884|199||ĺ sama hraunlagi og G-8 u.þ.b. 1.5 m ofar, en þar er bergið þéttara en nokkuð sprungið. |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|4.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-10|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|674158|441312|-15.38319|64.42886|199||Sama hraunlag og G-9 en nú borað ofan á topp hraunlagsins s.s. hornrétt á G-9 en samsíða 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|2.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.0|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-11|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675256|442208|-15.35937|64.43632|414||Úr líparíteiningu 1. Dæmigert straumflögótt ljóst og smáblöðrótt. |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|14.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|14.7|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|||||||||||||||
G-12|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675625|442316|-15.35160|64.43709|455||Móbergsbreksía úr móbergseiningu 1. Bergið er grágrænt á lit, minnir einna helst á þursaberg 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|18.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.5|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|||||||||||||||
G-13|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675631|442327|-15.35145|64.43719|455||Grágrænt túff úr móbergseiningu 1.  Bergið líkist mjög því sem kallað er móbergsset vegna samlímdra smárra korna, þau stærstu all tað 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|34.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|34.2|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|||||||||||||||
G-14|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|10.8.1992|Surface|Geitafellsgil|675708|442388|-15.34979|64.43769|455||Straumflögóttur auðboranlegur líparítgangur. Gangurinn er víðast um 1-2 m á þykkt og liggur í stefnu gilsins, þ.e. 25°. Sýnin voru tekin samsíða 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|23.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|23.4|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|||||||||||||||
G-15|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675165|439392|-15.36462|64.41114|87||Basalteining 1a.  Bergið er mjög þétt og a.m.k. 10 m þykkt, skorið af göngum úr fasa 5. Bergið er smásprungið.|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|2.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-16|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675167|439411|-15.36456|64.41132|90||Basalteining 1a. Fínkornótt þóleiíthraun ljósgrænt á lit og sprungið milli keiluganga. Borað 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|22.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|21.8|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|||||||||||||||
G-17|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675174|439414|-15.36439|64.41134|91||Basalteining 1a. Tekið úr sama lagi og G-16 en tekið úr ferskari hluta þess. Ath. Sýnin voru nokkuð dreifð í laginu vegna erfiðleika við að ná A-sýni, en þau 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|1.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-18|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675232|439434|-15.36318|64.41149|94||Basalteining 1a. Fínkornótt blöðrótt en þétt og dílótt þóleiíthraunlag. Blöðrur 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|1.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-19|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675245|439433|-15.36291|64.41147|94||Basalteining 1a. Tekið úr sama hraunlagi og G-18, en nú borað lóðrétt niður í efri hluta þess þ.e. hornrétt á G-18. Hraunlagið um 3 m á þykkt og sýnið tekið 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|10.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|9.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-20|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675244|439445|-15.36291|64.41158|95||Basalteining 1a. Borað í þéttan karga milli hraunlaga, innsta kosti 2 m þykkur grágrænn á lit með 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|5.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|5.1|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|||||||||||||||
G-21|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675235|439473|-15.36306|64.41183|99||Basalteining 1a. Borað í stein í gilinu, sem er eins og hraunlögin fyrir ofan. Það var gert vegna mikillar frostveðrunar og þar af leiðandi myndunar á þunnum flögum við yfirborðið. Hraunlagið er mjög blöðrótt grænt 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|2.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-22|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|11.8.1992|Surface|Kráksgil |675243|439474|-15.36290|64.41184|99||Basalteining 1a. Í mynni Kráksgils. Borað í ljósgrænt ummyndað basalt með epidót, granar og aktínoólít í. Steinn var tekinn úr því til að bora í, þar sem allt bergið var sprungið og flögótt vegna frosveðrunar. |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|16.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.3|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|||||||||||||||
G-23|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677656|442572|-15.30919|64.43833|277||Móbergseining 2. Sýni tekið við efri mörk á grænu túffi eða þar sem litaskipti eru yfir í brúnt. Ath. Vergið sýnir víðast hvar einkenni móbergssets, þ.e. samlímdir smá molar í þessu tilviki kantaðir. Ekki tókst að ná almennilegum kjarna A og var því 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|||||||||||||||||||||||
G-24|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677631|442561|-15.30971|64.43824|291||Móbergseining 2. Brúnt túff með smábrotum og vel samlímt og er neðan við græna beltið. Rétt ofan við eru dreifðir bólstrar í móberginu með ásýnd eins og um dílótt basalthraun væri að ræða. Bólstranir hafa verið tengdir innbyrðis með sprungum og er lámontít aðal ummyndunarsteind í þeim.|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|21.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-25|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677614|442552|-15.31009|64.43817|299||Móbergseining 2. Borað í fínkornótt set með hvarfleirs einkenni. Gæti verið 10-20 m þykkt. Það fær túfflegri ásýnd ofar. Athuga ber að staðurinn er utan við 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|22.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|21.7|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|||||||||||||||
G-26|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|19.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.8|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|||||||||||||||
G-27|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 neðar í þéttari hluta lagsins, en það er 1-2 m á þykkt 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|7.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.6|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|||||||||||||||
G-28|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677548|442528|-15.31147|64.43799|330||Basalteining 2. Borað í breksíu milli hraunlaga, fyllta af zeólítum. Lagið er þykkt með þunnu stáli en þykkri 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|16.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|16.6|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|||||||||||||||
G-29|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677522|442524|-15.31202|64.43797|342||Basalteining 2. Sýni tekið úr bergstáli í þéttu fínkorna basalti 5m þykku með 1-2 m þykkri breksíu fyrir ofan og neðan. Sýnið sennilega tekið 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|1.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-30|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677494|442528|-15.31260|64.43802|353||Basalteining 2. Sýni tekið úr þéttu fínkorna þóleiítbasalthrauni. Það sést nokkra metra þykkt stál með vel þjöppuðum 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|0.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-31|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Námagil í Hoffellsdal|677522|442515|-15.31203|64.43789|342||Móbergs- eða basaltbreksía, sem stratigrafískt tilheyrir H-I einingu, en opnan hér í Námugili er nokkuð þunn, og hraunlög sem tilheyra B-II ofan við og B-I neðan við. Kjarninn er tekinn úr millimassa efni í breksíunni (því annars værum við í basaltsteini). Súr bergbrot sjást í breksíunni líka. Vera má að þetta 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|2.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|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|||||||||||||||
G-32|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 að vera á mörkum blandlags- og klórítbeltis í ca 150 m y.s. Borað er í þéttan hluta hrauns sem er brúnveðrað, fínkornótt þóleiít, 4-5 m þykkt. |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|1.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-33|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|12.8.1992|Surface|Hoffellsfjall milli Skoru og Segils|677926|441128|-15.30534|64.42526|256||Feldsat dílótt þunnt hraun (1 m þétt, 1 m kargi). Kjarninn er boraður hornrétt á flæðilegu í þéttan 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|2.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-34|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Hoffellsfjall milli Skoru og Segils|677935|441127|-15.30514|64.42524|247||Úr karganum á næsta hrauni neðan við, eða úr blöðrótta 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|4.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.7|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|||||||||||||||
G-35|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Stóraskriðugil|677505|439292|-15.31629|64.40904|222||Stóraskriðugil, í klórítbelti fremur en blandlagsbelti.  Þétt fínkornótt þóleiít hraun, 5-6 m þykkt, með 1 m kargalagi ofaná. Kjarnarnir eru boraðir inn í hraunið samsíða flæðiböndum, 1 m ofan við botns hraunsins. |Stóraskriðu 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|1.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-36|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Stóraskriðugil|677497|439297|-15.31645|64.40909|229||Borað í blöðróttan efri hluta sama hrauns og G-35. Blöðrótti hlutinn er ca. 1.5-2 m á þykkt og er kjarninn tekinn 30-40 cm ofan þétta 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|13.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|5.4|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|||||||||||||||
G-37|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Stóraskriðugil|677507|439302|-15.31622|64.40912|221||Sama hraun og G-36/36 en ca 1 m ofan þétta hlutans. Þétta sýni er áberandi blöðróttara 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|16.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|16.9|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|||||||||||||||
G-38|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Stóraskriðugil|677514|439300|-15.31609|64.40910|216||Þétt þóleiít hraun ca 4 m þykkt með 1 m karga. Sýnið er tekið ca 1 m frá botni til samanburðar við G-35 í sama klóríðbelti. Blöðrur sjást vel með berum augum og prímer groppa því líklega hærri. Epidót sést ekki í sýninu en aðeins vottar fyrir því í lausu kargaefni í farvegi þessa 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|1.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-39|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Stóraskriðugil|677560|438699|-15.31586|64.40369|70||Súrt rhyolít hraun úr botni B-I myndunnar. Fullt af epidóti. Sýnið var tekið 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|7.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|7.0|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|||||||||||||||
G-40|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|13.8.1992|Surface|Geitafellsgil í mynni gilsins|673839|440346|-15.39094|64.42037|84||Geitafellsgabbró. Sýni tekið úr Geitafellsgabbóri, sem er innskota fasi 2 í eldstöðinni. Borað var í laust grjót úr grjótnámu (Seðlabankinn). |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|0.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-41|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 meðalgróft og blöðrur 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|4.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.4|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|||||||||||||||
G-42|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 með aðliggjandi granófýr. Gangurinn er blöðróttur. |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|1.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-43|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673823|440421|-15.39119|64.42105|87||Sýni tekið úr 60 cm þykkum gangi, sem var dílóttur inn við miðju. Sýni var tekið utan við 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|2.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-44|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil í mynni gilsins|673815|440422|-15.39135|64.42106|86||Sýni tekið 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|1.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-45|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkur og blöðróttur við kæliflötinn 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|1.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-46|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þvert á ganginn í gegnum blöðróttan jaðar.|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|1.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-47|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkur. Berið er dílótt og útfellingar í sprungum. Gangaþéttleiki 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|2.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|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|||||||||||||||
G-48|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673826|440846|-15.39062|64.42486|135||Sýni tekið úr dólerítgangi, sem tilheyrir fasa 7. Gangurinn er dílóttur inn að miðju, en hann er um 1.5 m á þykkt. Sýni tekið úr hlið hans þar sem fylla hefur brotnað 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|2.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.8|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-49|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673825|440850|-15.39064|64.42489|136||Sýni tekið úr keilugangi úr fasa 5. Gangurinn er yfir 1 m á þykkt. |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|3.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.1|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|||||||||||||||
G-50|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673825|440857|-15.39064|64.42495|137||Sýni tekið úr dulkornóttum gangi sem hríslast ofan  við G-49 og er 5-15 cm þykkur. |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|1.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-51|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673826|440865|-15.39061|64.42503|139||Sýni tekið úr keilugangi, sem tilheyrir fasa 5. Steinn var tekinn úr ganginum og boraður.|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|7.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.8|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|||||||||||||||
G-52|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|14.8.1992|Surface|Geitafellsgil|673832|440867|-15.39048|64.42504|141||Sýni tekið úr 1.5 m þykkum gangi úr fasa 5,  rétt við 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|2.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.1|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|||||||||||||||
G-53|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkur og er annar jaðarinn að minnsta kosti mikið 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|6.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.2|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|||||||||||||||
G-54|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkt. |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|5.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-55|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkt og sker móberg en rétt við 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|1.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|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|||||||||||||||
G-56|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670965|443417|-15.44690|64.44933|165||Sýni tekið úr sama gangi og G-55 en nú við jaðar hans. Ath. Gangurinn er mikið brotinn og liggja æðar langs og þvers.|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|2.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.4|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|||||||||||||||
G-57|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670952|443399|-15.44719|64.44918|167||"Líklega ""feeder dyke"" og þá fasi 1. Smá stubbur sést af honum í móbergsmyndun 2 og er 1 m á þykkt. Epidót sést á kæliflötum og súlfíð 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|3.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-58|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670949|443368|-15.44730|64.44891|168||Móbergseining 2. Sýni tekið skammt frá G-57 og rétt við fasa 11, sem er súr. Bergið er mjög túfflegt. Þetta er rétt við jökuljaðarinn. |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|9.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|8.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-59|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkur og var sýnið borað úr hlið hans. Hann er fínkornóttur, blöðróttur, stakdílóttur og sést epidót í þeim.|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|0.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-60|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670939|443339|-15.44753|64.44865|169||Dólerítkeilugangur, sem tilheyrir fasa 5. Sýni var borað þvert á hann að ofanverðu. Mikið kraðak var af flestum Innskotafösunum þarna 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|2.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-61|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670934|443330|-15.44765|64.44857|169||Sýni úr keilugangafasa 6. Hann er pofrýrískur og u.þ.b. 1 m á þykkt. Sýnið var tekið þvert á stuðlun.|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|3.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.0|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-62|Sigurðsson and Stefánsson, 1994|Guðmundsson 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, grænleitur að sjá og epidótríkur. Epidót virðist korna í stað plagíóklas í dílum. Sýni var tekið í gegnum jaðar gangsins samsíða stuðlun.|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|3.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.0|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-63|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670918|443299|-15.44801|64.44830|171||Handsýni var tekið úr súrum gangi til þess að bora í bænum. Sýnið nokkurn veginn úr miðjum ganginum, en hann er nokkra metra þykkur (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|2.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.7|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-64|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670920|443275|-15.44800|64.44808|172||Dólerítgangur, sem tilheyrir fasa 12. Sýnið er tekið nokkurn veginn í miðjum ganginum, sem er um 4 m þykkur. Utan í ganginum eru 10-40 cm þykkar æðar af kalsíti, kvarsi og súlfíðum.|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|4.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-65|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670920|443272|-15.44801|64.44806|172||Sýni tekið tekið í 0.5-1 m breiðri sónu á jaðri dólerítsgangsins, sem sýni G-64 var tekið 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|0.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-66|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670912|443258|-15.44819|64.44794|172||Basaltbreksía líklega tengd hraunlögum, en erfitt er að meta þykkt þeirra. Sennilega fáeinir metrar á þykkt. |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|2.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-67|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Gjátungur|670901|443258|-15.44843|64.44794|173||Sýni tekið um 5m ofan við G-66 í fínkornóttu basalt hraunlagi, en það er fínblöðrótt og þær 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|0.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-68|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Innst við Þverá austan Efstafellsness|672082|442610|-15.42470|64.44154|223||Sýni tekið úr bergstáli fínkorna þóleiítshraunlags, en skammt frá sýnatökustaðnum er 20-40 cm þykk kalsítæð. |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|1.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
G-69|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|15.8.1992|Surface|Norðan Kráksgils|675118|439360|-15.36564|64.41088|79||Hraun úr basalteiningu B-I rétt norðan Kráksgils í aktínólít belti.  Hraunið er þétt ásýndar, þóleiít, 4-6 m þykkt, fínkornótt. Borað var í mitt hraunið samsíða flæði (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|0.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-1|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361550|442011|-21.87706|64.45156|172||Hraunlag undir eða á milli dólerít keiluganga. Bergið er fínkorna,  blöðrótt, ljósgrænt í brotsári. Blöðrur 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|13.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|13.4|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|||||||||||||||
H-2|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361550|442011|-21.87706|64.45156|172||Keilugangur (hæð 105 m y. s.), um 5 m ofan við hraunlagið. Bergið er fín-meðalkorna 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|3.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-3|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361562|442031|-21.87683|64.45175|180||Grannberg við 1 m þykkan keilugang (H-2) að ofanverðu. Bergið er fínkorna, ljósgrágrænt, blöðrótt og blöðrufyllt af a: svörtum leir > klórít, b: Hvítar fyllingar með epidóti og etv granati. Bergið 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|14.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|14.2|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|||||||||||||||
H-4|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361591|442056|-21.87625|64.45198|193||Gabbró eða grófkorna dólerít keilugangur, flögótt berg (hæð 115 m).  Fyrsta haftið í gilinu. Bergið grá-grænleitt. |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|2.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.7|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|||||||||||||||
H-5|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361603|442071|-21.87601|64.45213|201||Kolummyndað hraunlag milli keiluganga. Grænleitt að lit, fínkorna, blöðrótt. Epidót, granat? Og magnetít. Bergið 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|16.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.8|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|||||||||||||||
H-6|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361624|442095|-21.87559|64.45234|213||Keilugangur (150m hæð). Hlíðarnar mjög skriðuorpnar og lítið að sjá annað en keiluganga með reglulegu millibili. Keilugangurinner um 1 m breidd, grófkorna og grár að lit. Feltmynd sem sýnir afstöðu 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|1.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.3|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|||||||||||||||
H-7|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361620|442086|-21.87567|64.45227|209||Mjög blöðrótt hraunlag rétt við kontaktinn á keiluganginum (sem sýni H-8 er tekið úr). Bergið er grænt að lit. Hvítar blöðrufyllingar en gulur blær bendir til viðveru epidóts. Bergið fínkorna grátt. Gæti verið við 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|10.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|10.1|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|||||||||||||||
H-8|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361620|442086|-21.87567|64.45227|209||Keilugangur, borað ofan í miðju hans. Gráleitt meðal-grófkorna og líklega plagíóklasdílótt. Ca. 1 m þykkt.|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|3.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.6|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|||||||||||||||
H-9|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361628|442091|-21.87552|64.45231|212||Hraunlag milli keiluganga. Fínkorna og þétt og smásprungið grátt að lit. Sýnið tekið rétt ofan við 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|4.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-10|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361735|442248|-21.87346|64.45377|282||Borað ofan í fínkorna þétt basalt í hornfels-sónu. Um 1 m neðan við keilugang. Smásprungið og smáblöðrótt og grásvart að lit. Ekki unnt að geta sér til um þykkt vegna kelugangnakraðaks. |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|7.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|7.0|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|||||||||||||||
H-11|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361744|442259|-21.87326|64.45387|286||Hraunlag úr hornfelsummyndun í komplex af göngum og keilugöngum (hæð 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|1.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-12|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361752|442269|-21.87312|64.45396|289||Gangur strik 30-35° með 60-70° austlægum halla og 1-1.5 m að þykkt. Þétt 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|||||||||||||||||||||||||||
H-13|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361780|442289|-21.87254|64.45414|296||Fínkornótt blöðrótt hornfels basalt í gangakomplex eins og H-12, en þetta er austan við  N-S gangana, sem lækurinn liðast eftir. Bergið er mjög ummyndað í kringum blöðrunar, er dökkgrænt í blöðrum en lýsist út frá þeim. |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|0.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.4|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|||||||||||||||
H-14|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361802|442277|-21.87207|64.45405|292||Gabbró áður en það verður grófast, mætti kalla meðalkorna (hæð 250 m). Þétt sprungulaust gabbró, grænleitt í annan endann, etv. vegna yfirborðsveðrunar.|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|2.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.2|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|||||||||||||||
H-15|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361811|442280|-21.87190|64.45408|293||Gabbró um 10 m ofar en H-14. Þétt blöðrulaust 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|1.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.6|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|||||||||||||||
H-16|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361816|442286|-21.87179|64.45413|295||Fínkorna gabbró í 230 m hæð 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|0.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-17|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361863|441239|-21.86984|64.44478|92||Fínkorna þóleiít hraunlag, Mjög flögótt, svipað og H-18 hvað varðar þykkt 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|3.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-18|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361874|441266|-21.86963|64.44502|94||Fínkorna grásvart þóleiít hraunlag, Þétt en blöðrótt til jaðranna. Lágmarksþykkt 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|3.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.7|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-19|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361876|441269|-21.86959|64.44505|94||Blöðrótt þóleiít hraunlag, ca. 2 m frá toppi, en þar eru laggangar. Bergið er grágrænt og verulega ummyndaðra en í sýninu á undan. Klórít, epidót, lámontít o.fl. Þykkt >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|4.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-20|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361883|441278|-21.86945|64.44513|94||Samskonar sýni og H-19. Mjög smáblöðrótt, 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|5.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|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|||||||||||||||
H-21|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361959|441316|-21.86792|64.44550|97||Hraunlag, borað um 1.5 m frá toppi lags sem er a.m.k.. 2.5 m þykkt en ekki sést í botninn. Um 1.5 m fyrir ofan er um hálfs metra þykkur laggangur. Bergið er blöðrótt. |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|5.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-22|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361959|441321|-21.86793|64.44555|97||Kargi ofan á laggangi. Ath. veðrun kargans ávöl líkt og sést í ólivín þóleiít en aftur á móti er veðrun hraunanna mjög þóleiítleg.  Karginn er nánast svartur, en víða verður hann snögglega ljósgrænn 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|3.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.9|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|||||||||||||||
H-23|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361974|441352|-21.86765|64.44583|99||Í um 2 m þóleiítkarga ofan á 3-5 m þykku 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|17.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.0|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|||||||||||||||
H-24|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361976|441360|-21.86761|64.44590|100||Í 3-5 m þykku þóleiít hraunlagi ofan á hraunlagi sem H-23 var tekið 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|3.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|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|||||||||||||||
H-25|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361984|441371|-21.86745|64.44600|101||Mjög svipaðar aðstæður og í H-23 en ekki eins skýrar vegna skriðu. |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|8.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|8.4|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|||||||||||||||
H-26|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.8.1992|Surface|Innan öskjunnar við Leirá|361986|441377|-21.86742|64.44606|102||Smáblöðrótt að 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|2.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|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|||||||||||||||
H-27|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Votuklettagil upp að Hrossatungugabbrói|361439|448364|-21.88538|64.50844|197||Súrt setlag rétt ofan við gömlu vatnsveitu Borgarness. Mjög flögótt, og í því má sjá kúluummyndun, þ.e. dökkgráleitar kúlu eða rákir sem raða sér línulega og hafa meiri ummyndun en ljósara bergið í kring. Ljósgrænt sýni tekið úr steini í skriðunni. 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|19.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|19.0|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|||||||||||||||
H-28|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361426|448314|-21.88561|64.50800|200||Blöðrótt fínkorna basalt nálægt toppi. Opnur í lagið takmarkaðar (130 m hæð). Töluvert sést af zeólítum í blöðrum, 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|10.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|9.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-29|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361428|448316|-21.88557|64.50801|199||Tekið úr hraunlagi í lækjarfarvegi skammt ofan við H-28 (130 m). Borað rétt við innskot og hluti sýnis gæti verið 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|5.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-31|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 (hæð 140 m). Stefna 20°. Allt að 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|2.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-32|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448097|-21.88611|64.50603|214||Gangur svipaður og H-31. Tekið úr miðju hans. Stakblöðrótt 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|||||||||||||||||||||||||||
H-33|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448074|-21.88609|64.50583|218||Mjög klórítfyllt hraun, blöðrótt og með epidóti. Sýnið sennilega tekið í efri hluta hraunlagsins. Sýnastaðurinn er rétt ofan við 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|0.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-34|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361394|448046|-21.88601|64.50558|221||Blöðrótt berg líkt og hraunlag um 1 m  NV við ganginn í H-31 ca. Nokkuð blöðrótt 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|1.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-35|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361393|448044|-21.88604|64.50556|222||Inni í miðjum ganginum. Þétt-smáblöðrótt 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|1.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-36|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361393|448035|-21.88602|64.50548|223||Gangur. Í H-36 er gangurinn smáblöðróttur og í kjarnanum eru þær fylltar klóríti. Mjög smáblöðrótt og þær 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|1.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-37|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361392|448021|-21.88604|64.50536|226||Borað í hraun í ca. 1 m fjarlægð frá gangi. Bergið er fínkorna og þétt og engar blöðrur (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|3.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-38|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361390|448008|-21.88607|64.50523|229||Keilugangur strik 120°, um 1 m að þykkt. Þétt, blöðrur sjaldgæfar og þá 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|7.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|7.3|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|||||||||||||||
H-39|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361314|447831|-21.88747|64.50362|266||Sýni tekið úr miðjum laggangi sem liggur á milli tveggja hraunlaga. Gangurinn um 40-50 cm þykkur. Þétt 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|2.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-40|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361310|447830|-21.88755|64.50361|267||Efra yfir borð á hrauni rétt fyrir ofan H-39. Virðist stakblöðrótt 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|2.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-41|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361305|447818|-21.88765|64.50350|271||Breksía ofan á hraunlagi, grænleitt að lit smásprungið.  Bergið er dökkt að sjá en við blöðrur og sprungur lýsist það mjög vegna aukinnar ummyndunar. Ath. ekki unnt að sjá þykkt hraunlagsins þar sem það sést aðeins ofan á það í klöppinni. Erfitt að 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|4.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.7|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|||||||||||||||
H-42|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361298|447816|-21.88780|64.50348|276||Borað í nánast það sama og í H-41 eða um 4 m norðar. Bergið er breksíukennt að sjá (um 200 m hæð). Blöðrulaust, mikið sprungukraðak 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|5.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.0|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-43|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361294|447783|-21.88785|64.50318|285||Yfirborð á hrauni. Hluti kjarnans er oxaður, þeir eru mjög blöðróttir með ljósgrænum leir í blöðrum. Mjög blöðrótt og fyllt, margar sprungur, óreglulegar, ein þeirra 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|3.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-44|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361292|447773|-21.88788|64.50309|289||< 6 m þykkt hraunlag, nærri 50 cm þykkum gangi. Bergið er smáblöðrótt. |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|1.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|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|||||||||||||||
H-45|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361284|447766|-21.88805|64.50302|295||Borað í setlag milli fínkorna hraunlaga. Setlagið er lagskipt og fínkorna mjög (hæð 210 m). Líklegast kargi, mjög blöðrótt, 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|9.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|9.7|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|||||||||||||||
H-46|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361278|447748|-21.88815|64.50286|302||Borað er í ljósa ummyndun í breksíu nærri yfirborði 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|4.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-47|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361278|447745|-21.88816|64.50283|303||Borað í hraunlag, það sama og H-46, og er 0.5-1.0 m neðan þess. Bergið er fínkorna og enn nokkuð breksíulegt. Bergið er mjög epidótríkt. Smáblöðrótt, 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|2.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-48|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361275|447739|-21.88820|64.50278|305||Borað í epidótríka sónu í basalti, þ.e. sama basalti og í H-47 en litlu neðar í læknum. 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|10.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|10.5|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|||||||||||||||
H-49|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361274|447740|-21.88823|64.50279|306||Borað rétt ofan við neðri lagmót í 8 m þykku plagíóklas dílóttu hraunlagi. Þetta er rétt fyrir utan öskjujaðarinn. Hæðarmælir í 235 m. Smáblöðrótt og fyllt (einkum með 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|2.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-50|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361272|447740|-21.88826|64.50279|306||Breksía neðan sýnis H-49 og er líklegast karginn úr hraunlaginu fyrir neðan. Nokkuð blöðrótt fyllt, sprungukraðak, en mjög smáar, nema 2-3 sem viðast opnari nærri yfirborði.|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|1.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.0|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-51|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361272|447726|-21.88826|64.50266|310||Gulleit súr breksía í lækjarfarvegi um 2-3 m innan við öskjujaðarinn. Sýnið mjög ósamleit. Smávegis ófyllt holrymi á staka stað. Sprungunetskraðak undir mesmegnis 45° horni. Sumar viðast opnar við yfirborð 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|10.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|10.2|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|||||||||||||||
H-52|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361269|447709|-21.88831|64.50251|314||Fínkorna gangur á öskjujaðri, mjög ummyndaður grágrænn að lit. Blöðrulaust. 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|4.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|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|||||||||||||||
H-53|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361267|447700|-21.88833|64.50243|317||Borað í grófgerða basaltbreksíu í lækjarfarvegi ca. 30-40 m ofan og innan við kalderujaðarinn. Mjög blöðrótt 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|12.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|12.4|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|||||||||||||||
H-54|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361264|447695|-21.88838|64.50238|319||Súr breksía í lækjarfarvegi aðeins ofan við kalderujaðar, og ca. 100 m innan við kalderujaðarinn (hæð skv. hæðarmæli 270 m). Breksían er gulbrún og svört?, etv. Gefur epidótið þessa ásýnd. Kjarnataka léleg. Þétt smáblöðrótt og fyllt, fjöldi sprungna (að 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|6.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-55|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þessari súru seríu (275m hæð), sem sést í ofanverðu gilinu innan kalderunnar. Holufyllt túff, sterk 45°  sprungunet, 2 þeirra 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|12.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|12.6|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|||||||||||||||
H-56|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|27.8.1992|Surface|Ytra-Seleyrargil I Hafnarfjalli|361255|447686|-21.88856|64.50230|324||Líparít Þar sem lagið sem borað var í í H-55 breytist úr setkenndu efni í kristallað ca. 10 m ofar. Stakar porur 90% fylltar, sprungukraðak. |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|14.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|14.0|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|||||||||||||||
H-57|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Flyðrunum í Hafnarfjalli|359840|447530|-21.91784|64.50032|243||Granófýr sýni tekið úr Flyðrunum í Hafnarfjalli úr hnullungi sem lá nærri veginum. Bergið hart og þess vegna tekinn hnullungur til borunar seinna. Bergið er mjög gropið, epidót í blöðrum, etv prímert? Nokkuð smáblöðrótt og ófyllt. Engar sprungur. |Granophyre sample taken from Flyðrur 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|6.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.4|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|||||||||||||||
H-58|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|354377|430328|-22.01434|64.34389|1||Boraður kjarni í 8-10 m  þykkt dílótt basalt rétt neðan við 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|1.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.8|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|||||||||||||||
H-59|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkur breksíeraður toppur eða botn á hraunlagi. Mjög zeólítíseraður (analsím og kabasít). Mjög blöðrótt og um 40% fyllt. A sýnið er minna blöðrótt en önnur sýni með 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|31.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|31.3|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|||||||||||||||
H-60|Sigurðsson and Stefánsson, 1994|Guðmundsson 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. Nær blöðrulaust 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|4.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.8|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|||||||||||||||
H-61|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355749|428318|-21.98400|64.32646|58||Þóleiít hraunlag um 8 m þykkt, sýnið tekið um 1 m ofan við botn lagsins og borað samsíða straumflögun. Bergið er fínkorna og þétt. Gamall steptur vatnsveitustokkur neðan lagsins. Staksmáblöðrótt, fylltar með 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|1.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-62|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355754|428313|-21.98391|64.32642|58||Sýni nærri toppi sama þóleiít hraunlags og H-61. Bergið smáblöðrótt. Karginn veðraður í burtu af laginu. Borað þvert á straumflögun. Ath. H-61 feltmynd gerð H-61 og 62. Smáblöðrótt, lerskán í blöðrum, ca. 40% fylltar (smærri blöðrunar fylltar, þær stærri allt niður 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|2.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.5|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|||||||||||||||
H-63|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355794|428292|-21.98307|64.32624|63||Þétt þóleiít hraunlag 10-15 m þykkt við hliðina á vatnsveitustíflunni. Borað um 1 m frá botni lagsins. Borað samsíða straumflögun. Blöðrulaust, 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|0.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-64|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355803|428289|-21.98287|64.32622|64||Fínkorna þóleiít hraunlag, nærri toppi sama lags og H-63 er borað í. Boraðsamsíða straumflögun, en hún er ekki áberandi í þessu lagi. Feltmynd af afstöðu H-63 og 64. Blöðrulaust, veðrunarfletir 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|1.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-65|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akrafjall, west side of mountain Berjadalsá|355764|428284|-21.98367|64.32616|59||Samlímt konglomerat. Stakar tómar blöðrur, 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|14.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|13.7|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|||||||||||||||
H-66|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 neðan og vestan við bæinn Innra-Hólm. Zeólítíserað. Setið er fremur fínt (túffkennt?) með stöku hnullungum. Sérstök ummyndun sem felst í áberandi ummyndunarsónum í kringum jarðhitaæðar. Sýni borað í dökka hlutann og minna ummyndaða. |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|18.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.7|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|||||||||||||||
H-67|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 setið óreglulegt að lit. Blöðrur smáar og virðast 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|27.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|22.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-68|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkt og liggur ofan á setlaginu. Mjög zeólítaríkt en blöðrur ekki fylltar heldur meira húð í blöðrunum. Kabasít, anasím, thompsonít og vottur af skólesíti, e.t.v. phillipsít. Stakblöðrótt >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|6.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|5.9|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-69|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358450|425893|-21.92590|64.30586|7||Tekið um 30 cm ofar í sama hraunlagi og H-68. Sýnið er mun blöðróttara. Mjög blöðrótt og minnstu blöðrur alveg fylltar (zeólítar) þær stærri >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|5.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.8|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-70|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Innri-Hólmur by the north coast of Akranes|358446|425886|-21.92596|64.30580|6||Tekið vestar í sama lagi og H-68 og 69. Mjög blöðrótt og zeólítíserað neðra borð hraunlagsins um 30 cm ofan lagmótanna. Mjög blöðrótt, analsím í blöðrum ca 40% fylltar, minni blöðrur fylltar en þær stærri minna fylltar, 3 sprungur, þar af ein opin við kjarnayfirborð. |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|9.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|9.3|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|||||||||||||||
H-71|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Kúludalsá to the south of Akrafjall|361654|427586|-21.86135|64.32234|23||Dílótt basalt vestan við ósa árinnar. Mesólít-skólesít belti. Borað í þétt berg. Karginn er óreglulegur þar sem sýnið er tekið. Að því virðist blöðrulaust, 3 sprungur undir um 70° horni. (Yfirleitt eru sprungur í kjarnanum taldar með hringferð um 2 cm kjarnabút og þeirra tölu deilt með 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|4.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.8|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|||||||||||||||
H-72|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Kúludalsá to the south of Akrafjall|361644|427577|-21.86155|64.32226|23||Hraunlagið ofan H-71 og vestan. 6-8 m þykkt dílótt eins og síðasta sýni. Nokkuð smáblöðrótt og fylltar með dökkum leir, sprungulaust. Stór blaðra (1 cm) aðeins 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|3.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|3.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-73|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Ferro-alloy plant in Grundartangi|365273|430685|-21.78942|64.35157|5||Basaltlag niðri í fjöru beint fyrir neðan verksmiðjuna. Stórblöðrótt plagíóklas dílótt líklegt þóleiít í skólesít-mesólítbelti. Stakblöðrótt að mestu fylltar, 3 sprungur með 90°. Sterk straumflögun (þóleiítleg) 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 (þóleiítleg) with a 0° dip.|Lava flow|Porphyritic basaltic lava|Smectite-zeolite|2.99|Measured on crushed sample by Western Atlas Borehole Laboratories|3.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.9|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|||||||||||||||
H-74|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akranes, between the lighthouses on Skipaskagi|350289|426546|-22.09500|64.30823|0||Ólivín þóleiít hraunlag. Sýnið tekið á klöpp á milli vitanna á Skipaskaga. Hraunlögin líklega innan dyngju. Með 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|2.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.4|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-75|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|Akranes, between the lighthouses on Skipaskagi|350268|426592|-22.09547|64.30862|0||Borað ofan í ólivín þóleiít hraun við nýja vitann. Samskonar hraun og H-74. Stakblöðrótt, 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|1.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-76|Sigurðsson and Stefánsson, 1994|Guðmundsson 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||Borað í sama berg nær suður eða suðaustan við skreiðarhjalla HB. 1 fyllt blaðra, 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|2.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-77|Sigurðsson and Stefánsson, 1994|Guðmundsson 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||Fært sig um 5 m í átt að sjónum og borað í sama lag en mun blöðróttara en H-76. 2 smáar blöðrur, 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|3.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|2.5|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|||||||||||||||
H-78|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|The beach to the east of Ytrihólmur|353410|425745|-22.02977|64.30240|3||Ólivín þóleiít basalt úr dyngju. Grófkorna ólivín þóleiít, blöðrulaust, 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|5.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|5.3|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|||||||||||||||
H-79|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 borað í fremur þéttan hluta lags. Blöðrulaust, 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|7.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|7.2|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|||||||||||||||
H-80|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|28.8.1992|Surface|The beach to the east of Ytrihólmur|353594|425752|-22.02599|64.30254|5||Dyngjubasalt, sama og síðasta sýni nema blöðróttara. Ca, 10 m austan við H-79. Nær blöðrulaust, grófkorna ólivín þóleiít, 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|4.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|4.6|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
H-81|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the north side of the mine|382857|434487|-21.42877|64.39215|28||Rhyolít. Líparít kubbabergsbólstri, sýni tekið úr miðju stuðuls. Ummyndun óljós í felti og var því látið bíða 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|||5.6|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|||||||||||||||
H-82|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the north side of the mine|382795|434482|-21.43004|64.39208|27||Líparít breksía. Sýni tekið úr steini við ána, norðan við 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|||24.2|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|||||||||||||||
H-83|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the north side of the mine|382861|434489|-21.42868|64.39217|29||Rhyolít-kubbaberg? Súlfíðsóna í sama líparíti og á undan í sprungusónu. Bergið 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|||1.5|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|||||||||||||||
H-84|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the north side of the mine|382861|434489|-21.42868|64.39217|29||Rhyólít. Sami þursabergseitill og á undan sýni tekið um 4 m frá H-83 að því er virðist í ferskari hlutanum. Kubbabergseitlarnir eru 10-20 m langir og ca. 4-6 m háir (ónákvæmt). |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|||7.2|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|||||||||||||||
H-85|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the north side of the mine|382857|434501|-21.42878|64.39228|31||Rhyolíttúff. Blöðrótt fremur hart berg og eru blöðrur tómar. Ath. H-81-85 eru tekin að norðanverðu 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|||||||||||||||||||||||||
H-86|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hvalfjörður, Líparite quarry, on the south side of the mine|382857|434501|-21.42878|64.39228|31||Rhyolíttúff. Sýni tekið í sunnanverðri námunni í mjög ummynduðu 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|||18.6|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|||||||||||||||
H-87|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382881|435448|-21.42903|64.40077|97||Rhyolítbreksía, þ.e. súrt túff með líparít og biksteinsbrotum í. Ummyndun en kabasít sést í blöðrum. (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|||18.3|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|||||||||||||||
H-88|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382890|435442|-21.42883|64.40072|97||Líparít eða rhyolít. Ljós drappleitt berg nokkuð þétt eða massíft. Ath. Sýni tekið 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)|||18.6|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|||||||||||||||
H-89|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Upper liparite quarry SR|382897|435439|-21.42870|64.40069|96||Líparít eða rhyolít. Sýni tekið úr ljósgrábrúnu fínkorna þéttu bergi. Ummyndun? Borað í bergstálið 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|||20.6|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|||||||||||||||
H-90|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|The beach in Hvalfjörður, near the village of Hrafnabjörg|378465|434913|-21.52008|64.39442|19||Dólerít, á Hvalfjarðarströnd í námu. Sýni af nokkuð ferklegu bergi.|Dolerite, on the Hvalfjörður 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|||0.5|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|||||||||||||||
H-91|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|The beach in Hvalfjörður, near the village of Hrafnabjörg|378455|434905|-21.52028|64.39435|19||Dólerít, u.þ.b. 20 cm sprungubelti í gegnum dólerítið. Ummyndun er nokkuð við sprungubeltið 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|||||||||||||||||||||||||||
H-92|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|||2.2|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|||||||||||||||
H-93|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 tekið úr ferskari hluta lagsins, en það er >6m á þykkt.|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|||0.4|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|||||||||||||||
H-94|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 tekið úr ummynduðum grænleitum hluta lagsins. Bæði sýnin eru tekin um 0.5 m ofan við 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|||4.5|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|||||||||||||||
H-95|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362439|448596|-21.86481|64.51093|182||Berggangur 1,5 m þykkur af þóleiítgerð, dílóttur. Strik 10° og halli 25° til austurs. Nokkuð um fínar óreglulegar kristallaðar æðar. Sýnatökustaður rétt neðan 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|||1.5|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|||||||||||||||
H-96|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|||18.3|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|||||||||||||||
H-97|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362418|448618|-21.86526|64.51112|179||Gangberg, bergið er meðalkorna þétt nokkuð ummyndað basalt. Stefna 56° og er lóðrétt. XRD -> Leir -> smektít/blandlag. Aldursröð: 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)|||1.6|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|||||||||||||||
H-98|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362420|448618|-21.86522|64.51112|179||Keilugangur mjög sprunginn og virðist ummyndaðri heldur en H-99. Strik 350°. Gerður úr ólvín-þóleiít. |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|||12.8|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|||||||||||||||
H-99|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362423|448616|-21.86517|64.51111|180||Gangberg. Basaltkeilugangur dílóttur, 1,5 m á þykkt mjög svipaður 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|||0.9|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||||||||||||||||||
H-100|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|8.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362440|448610|-21.86480|64.51106|184||Basalt keilugangur um 1 m á þykkt, mjög ummyndaður. 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|||10.8|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|||||||||||||||
H-101|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 öskjujaðri. Innskot um 100%. Strik 170° og halli 60°. Basaltgangur. Um 0,5 m fínkornóttur laggangur, smásprunginn. Sýni tekið úr jaðrinum. |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|||3.8|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|||||||||||||||
H-102|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362702|447486|-21.85829|64.50109|340||Gangberg (silla) fínkorna holufyllt þéttsprungið þóleiít basalt. Um 1 m á þykkt. |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|||1.5|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||||||||||||||||||
H-103|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362694|447466|-21.85844|64.50091|346||Gangberg (silla) fínkorna blöðrótt þóleiít basalt, sem liggur ofan á H-102 og er um 1 m á þykkt. |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|||2.5|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|||||||||||||||
H-104|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|9.9.1993|Surface|Hafnarfjall, Inner Seleyrargil|362691|447459|-21.85850|64.50084|348||Líparít innskot, óreglulegt á eða við öskjujaðarinn líklega um 1m á þykkt. Litur gulur og rauðgulur og blöðrur sjást í því. |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|||17.8|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|||||||||||||||
H-105|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 þykkt og er dílóttur. Er við lækinn í gilinu rétt við H-101 - 103 og er samsíða þeim. 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|||2.2|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|||||||||||||||
H-106|Sigurðsson and Stefánsson, 1994|Guðmundsson 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. Þykkt 50 cm. Stefna 20° og er lóðréttur. Sýnatökustaður er við fossinn vestan meginn, þar sem gilið 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|||16.6|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|||||||||||||||
H-107|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 að ræða grannberg milli keiluganga eða misgengisbreksía, ljósgrá á lit og súlfíðrík, u.þ.bþ 0.5 m á þykkt. Er við fossinn rétt neðan við 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|||21.4|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|||||||||||||||
H-108|Guðmundsson et al., 1995|Guðmundsson et al., 1995|9.9.1993|Surface|Inner Seleyrargil|362658|447882|-21.85958|64.50463|257||Basalthraun. Efri hluti hraunlags fín-meðalkorna líklega þóleiít basalt. Bergið er ljós grænt af ummyndun, holufyllt og blöðrótt. Pýrít og amfiból sjást. Sýnatökustaður ca. 20 m frá H-107. Teknir voru sérkjarnar af sprungufyllingum, dökkgrænir 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|||9.3|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|||||||||||||||
H-109|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362658|447870|-21.85957|64.50452|259||Basalthraun, tekið úr miðhluta þess um það bil 20 m frá H-108. Bergið er fín-meðalkorna og blöðrótt.|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|||4.9|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|||||||||||||||
H-110|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362661|448034|-21.85967|64.50599|223||Blöðrótti hluti basaltlags, þ.e. á mótum tveggja basalthrauna. Erfitt er að dæma um þykkt laganna þar sem ekki sést í botn né topp þeirra vegna skriðu og innskota. Sýnatökustaður um 4 m frá H-109. Pýrít sést og er mikið af því. Annars er bergið grænleitt 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|||11.2|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|||||||||||||||
H-111|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362662|448027|-21.85964|64.50593|225||Basalthraunlag, frekar þétt og meðalkorna og virðist klórítríkt. Staðsetning er beint fyrir neðan 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|||2.2|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|||||||||||||||
H-112|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362663|448013|-21.85960|64.50580|229||Basalthraun um miðbik hraunlagsins 1-2 m neðan við 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|||4.9|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|||||||||||||||
H-113|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362662|448006|-21.85962|64.50574|230||Basalthraun ofan við lagganginn í blöðróttari hlutanum nálægt 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|||3.0|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|||||||||||||||
H-114|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362671|447973|-21.85939|64.50545|241||Súr laggangur. Sýnið er tekið í læknum og er greinilegt að mikil ummyndun fylgir honum. Strik er 145° og halli 10° til austurs. Ath H-108 er ca 11m ofan við 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|||14.0|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|||||||||||||||
H-115|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362673|447967|-21.85936|64.50539|243||Basaltgangur eins meters þykkur. Gangurinn óreglulegur og sker súra innskotið (H-114) og er þéttur af sprungufyllingum. Pýrít er algengt (ath. Eldri ummyndun en sú súra). Erfitt að mæla strik innskotsins en það gæti verið 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|||1.2|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|||||||||||||||
H-116|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362671|447968|-21.85939|64.50540|242||Basaltkeilugangur um 1 m á þykkt og er fínkorna. Sýni tekð úr miðju 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|||0.5|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|||||||||||||||
H-117|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362670|447956|-21.85941|64.50529|244||Basaltkeilugangur um 1,5 m á þykkt og er fínkorna. Stilbítsprunga sést ofan við ganginn. Sýni tekð úr miðju 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|||4.0|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|||||||||||||||
H-118|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362666|447939|-21.85947|64.50514|247||Basalthraun. Mjög blöðrótt fínkorna basalt, sennilega toppur á hraunlagi. Ummyndun getur verið tengd órelulegum basaltgangi 2-3 m þykkum. Epidót er algengt og blöðrur eru leirfylltar. Í um 20 cm fjarlægð 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|||3.7|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|||||||||||||||
H-119|Guðmundsson et al., 1995|Sigurðsson 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 ummyndaður.|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|||7.2|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|||||||||||||||
H-120|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362688|447752|-21.85883|64.50347|287||Basalthraun. Toppur á mjög blöðróttu hraunlagi í árfarveginum. Staðurinn var rétt ofan við sveig á gilinu, þar sem lítill foss er. Ath. Toppurinn á hraunlaginu er í árfarveginum og eru því engar upplýsingar um þykkt lagsins, en lögin ofan við eru 6-8 m þykk.|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|||2.2|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|||||||||||||||
H-121|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362682|447732|-21.85895|64.50329|291||Basalthraun á sama stað og H-120, en fjær ummyndunarsónu við sprungurnar. Bergið virðist vera nokkuð þétt, þ.e. fínkorna smáblöðrótt. Klórít að mestu í blöðrum og það er með 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|||0.3|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|||||||||||||||
H-122|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362686|447564|-21.85871|64.50179|328||Basalthraunlag fínkorna og smáblöðrótt, mjög ummyndað þóleiít. Bergið er grænt - ljósgrænt á lít og sjást epidót, klórít, ef til vill granat (brúnleitur) ásamt hvítum torkennilegum útfellingum. Sýni tekið á stalli við svigðu í um 280 m hæð skv. Hæðamæli.|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|||4.5|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|||||||||||||||
H-123|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362692|447574|-21.85858|64.50187|325||Basalthraun, fínkorna af þóleiít gerð grágrænt á lit. Sýni sennilega úr miðbiki lagsins, við hliðina 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|||3.4|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|||||||||||||||
H-124|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362648|448073|-21.85997|64.50633|210||Dólerítgangur 3 m þykkur grófkorna basalt sambærilegur við fasa 12 í Geitafelli. Hæðarmælir sýnir 210 m á sýnatökustað. 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|||2.7|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|||||||||||||||
H-125|Guðmundsson et al., 1995|Sigurðsson 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 miðju 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|||7.9|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|||||||||||||||
H-126|Guðmundsson et al., 1995|Sigurðsson et al., 2000|9.9.1993|Surface|Inner Seleyrargil|362645|448064|-21.86002|64.50625|208||Basalthraun, fínkorna smáblöðrótt og ummyndun líklega í smektít beltinu. Sýnatökustaður 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|||4.6|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|||||||||||||||
H-127|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365816|449959|-21.79584|64.52450|47||Basalthraun,  fínkorna og þétt þóleiítbasalt. Lagið er 8-10 m þykkt. Sýnataka  í mynni gilsins að 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|||1.7|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|||||||||||||||
H-128|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365865|449940|-21.79479|64.52435|52||Basalthraunlag, sýni tekið úr blöðróttum 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|||7.9|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|||||||||||||||
H-129|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365870|449922|-21.79467|64.52419|53||Líparít. Sýnatökustaður við botninn á neðsta líparítlaginu í Árdalsgili. Bergið er hnúðótt og eru þeir frekar massífir annars staðar var nánast vonlaust að 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|||4.1|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|||||||||||||||
H-130|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365867|449907|-21.79472|64.52406|54||Líparít. Sýni tekið um miðbik 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|||14.0|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|||||||||||||||
H-131|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365927|449781|-21.79335|64.52295|65||Basaltgangur, keilugangur 1,5 m þykkur fín-meðalkorna. Svipaður staður 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|||4.4|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|||||||||||||||
H-132|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365956|449748|-21.79272|64.52267|70||Líparít. Sýni tekið í flúðum í ánni og úr efri hluta sama lags og á undan. Bergið 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|||4.4|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|||||||||||||||
H-133|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365960|449756|-21.79265|64.52274|69||Líparít. Sýni tekið úr toppinum á líparítlaginu hér á undan með breksíulegt útlit en þétt og var sýnatökustaðurinn 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|||4.3|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||||||||||||||||||
H-134|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365959|449753|-21.79267|64.52272|69||Rhyolít, sýni tekið við hliðina 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|||7.7|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|||||||||||||||
H-135|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|365960|449750|-21.79263|64.52269|70||Súrt túff, ljósgrænt á lit og situr í bollum efst í líparítlaginu. Á sama stað 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|||18.5|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||||||||||||||||||
H-136|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|366007|449725|-21.79164|64.52249|76||Basaltgangur um 1 m þykkur af fín - meðalkorna þóleiíti. |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|||7.7|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|||||||||||||||
H-137|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|366343|449404|-21.78436|64.51974|120||Ignimbrít innst í Árdalsgili. Sýni tekið við hliðina á neðsta 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|||12.1|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|||||||||||||||
H-138|Guðmundsson et al., 1995|Sigurðsson et al., 2000|10.9.1993|Surface|Brekkufjall - Ársdalsgil in the area around Borgarfjörður|366353|449400|-21.78415|64.51971|123||Andesít stuðull laus í Árdalsá, óherilega hart að taka sýni. Stuðullinn er úr brekkunni þar 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|||0.4|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|||||||||||||||
H-139|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365916|442135|-21.78656|64.45443|528||Dacít pulsa úr bjargi rétt neðan við klettana vestan í Rauðahnjúk. Sýnið úr vel stuðluðu kubbabergi. |Dacite elongated entablature formation just below the cliffs west of Rauðahnjúkur.|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|||0.3|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|||||||||||||||
H-140|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365852|441885|-21.78766|64.45216|476||Líparít, blöðrótt straumflögótt og engin ummyndun greinanleg því þarf að láta XRD skera þar 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|||10.8|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|||||||||||||||
H-141|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365827|441668|-21.78799|64.45020|453||Basaltandesít, straumflögótt fín - dulkorna og þétt. Sýni tekið úr mosavaxinni skriðu neðan við klettabelti sunnan við Rauðahnjúk. |Basaltic andesite, flow-banded, fine-grained and dense. Sample taken from mossy skree below a cliff belt to the south of Rauðahnjúkur, |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|||0.3|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|||||||||||||||
H-142|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365673|441846|-21.79135|64.45174|463||Móbergsbreksía eða túff ljósgrænt til grænt á lit. Sýni tekið úr gili vestan Rauðahnjúks ofan við smá stall. |Hyaloclastite breccia or tuff, light-green to green in color. Sample taken from the gorge west of Rauðahnjúkur 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|||37.2|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|||||||||||||||
H-143|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365653|441844|-21.79175|64.45172|464||Gangberg. Sennilega fínkorna smásprunginn keilugangur, grár á lit. Hann liggur nokkuð óreglulega í gegn um túffið 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|||0.8|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|||||||||||||||
H-144|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365662|441842|-21.79156|64.45170|463||Líparítgangur um 10 m þykkur. Ummyndað túff er við jaðra 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|||15.8|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|||||||||||||||
H-145|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Skarðsheiði, to the north of Snók|365661|441837|-21.79159|64.45165|463||Basaltgangur um 0,5 m á þykkt og er smáblöðróttur. Hann sker líparítganginn. Strik 10° og halli 40° til vesturs. Ath. Sprungufyllingar í túffinu þarna í kring eru aðallega 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|||9.4|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|||||||||||||||
H-146|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Leirá|361835|440996|-21.87020|64.44259|82||Súrt túff, flögótt um 100-200 m utan við 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|||29.3|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|||||||||||||||
H-147|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Leirá|361829|440993|-21.87031|64.44255|81||Súrt túff. Ummyndað samskonar túff og H-146 með einhverri súlfíðvirkni Sýnatökustaður ca. 1m frá jarðhitasprungu 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|||19.8|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|||||||||||||||
H-148|Guðmundsson et al., 1995|Sigurðsson et al., 2000|15.9.1993|Surface|Leirá|361823|440987|-21.87043|64.44250|81||Gangberg. Gangurinn er meðalkorna ólivín þóleiít og sprunginn. Þykktin 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|||2.9|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|||||||||||||||
H-149|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373431|449365|-21.63684|64.52212|106||Basalthraun. Þunnlögótt fínkorna sprungið þóleiít, ca. 3m þykkt með 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|||2.5|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|||||||||||||||
H-150|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373420|449361|-21.63706|64.52207|106||Basalthraun. Næsta hraunlag ofan við H-149, sýni tekið úr hlutanum. Lagið er um 3 m þykkt.|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|||4.4|He Gas pycnometry, Geological Survey of Denmark and Greenland|||||9.87E-19|Measured by Geological Survey of Denmark and Greenland|||||||||||||||
H-151|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373429|449345|-21.63685|64.52194|107||Basaltkargi. Sýni tekið úr kargakenndum toppi sama lags og H-150 og er mjög sprungið. 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|||10.3|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|||||||||||||||
H-152|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373441|449330|-21.63661|64.52180|109||Basalthraun. Þétti hlutinn í næsta hrauni fyrir ofan H-151, einn fínkorna þóleiít og um 5 m þykkt. 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|||4.1|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|||||||||||||||
H-153|Guðmundsson et al., 1995|Sigurðsson 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 tekið í miðjum smáblöðróttum 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|||6.3|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|||||||||||||||
H-154|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373446|449313|-21.63647|64.52165|110||Basalthraun. Næsta hraun ofan á 153. Hraunlagið er ca. 6 m á þykkt. |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|||2.1|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|||||||||||||||
H-155|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373452|449299|-21.63634|64.52153|111||Basaltkargi. Sýni tekið 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|||19.3|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|||||||||||||||
H-156|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373455|449293|-21.63627|64.52148|112||Basalthraunlag. Næsta basaltlag ofan á H-155, þétt fínkorna þóleiít. Sýni tekið um 1 m ofan við kargann. Lagið er ca 6 m þykkt með 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|||1.2|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|||||||||||||||
H-157|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373468|449279|-21.63599|64.52136|113||Basaltkargi. Úr karganum ofan á H-156. Sýni tekið um 20 - 30 m sunnar við 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|||16.4|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|||||||||||||||
H-158|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skorradalshreppur|373478|449270|-21.63578|64.52128|114||Basalthraun. Næsta basaltlag ofan við H-157. Lagið er um 3 m þykkt.|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|||4.7|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|||||||||||||||
H-160|Guðmundsson et al., 1995|Sigurðsson et al., 2000|16.9.1993|Surface|Skarðsheiði|376061|448665|-21.58152|64.51681|203||Ignimbrít austan í Skarðsheiði. Steinn í árfarvegi rétt austan við skógræktargirðingar. Ummyndun er óviss.|Ignimbrite east of Skarðsheiði. 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|||7.3|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|||||||||||||||
H-161|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Dragháls|377828|448285|-21.54442|64.51405|96||Líparít-móberg við túff. Móbergsbreksía eða túff með 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|||21.9|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|||||||||||||||
H-163|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Dragháls|378283|451744|-21.53785|64.54522|272||Líparít úr gili í norðanverðum Skorradal gegnt Draga og austan Vatnsness. Bergið er blöðrótt og sýni tekið úr lausum stein sem ættaður er ofar úr hlíðinni sennilega alveg við 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|||8.8|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|||||||||||||||
H-164|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374612|436117|-21.60091|64.40382|10||Basalthraun. Blöðróttur 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|||9.0|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|||||||||||||||
H-165|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374623|436118|-21.60069|64.40383|10||Basalthraun, tekið úr þéttari hluta hraunlags H-164, sem er ca. 6m þykkt. 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|||2.1|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|||||||||||||||
H-166|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374629|436118|-21.60057|64.40383|10||Basalthraun. Neðri hluti fínkorna þétts hraunlags etv. blöðrótt um það bil 10 m frá H-165. Í því er 20 cm sprunga fyllt af kalsíti með 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|||4.3|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|||||||||||||||
H-167|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374636|436117|-21.60042|64.40383|10||Basalthraun. Tekið úr sama basaltlagi og H-166 og er rétt við áðurnefnda 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|||1.5|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|||||||||||||||
H-168|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374638|436117|-21.60037|64.40383|10||Basaltgangur. Keilugangur mjög sprunginn og ummyndaður, hallar til ausalægrar áttar um 15-20°. Ca. 1 m á þykkt. |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|||10.9|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|||||||||||||||
H-169|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374644|436120|-21.60025|64.40385|10||Sprungufylling. Tekið úr sprungu þeirri, sem sýni H-167 og H-166 standa við, að 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|||6.5|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|||||||||||||||
H-170|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374646|436120|-21.60021|64.40386|11||Basaltgangur, er 30 - 40 cm þykkur úr þóleiíti. Strik 140° og halli 10-20° til vesturs. Sýnatökustaður um 4 m vestan við 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|||0.5|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|||||||||||||||
H-171|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|374671|436121|-21.59970|64.40387|10||Súr gangur eða rhyolít um það bil 5 m þykkt. Ca. 100 m vestan hnitapunkts. Varasamt að 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|||14.1|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|||||||||||||||
H-172|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|375055|436082|-21.59171|64.40367|14||Basalthraun. Sýni tekið úr þéttari hluta lagsins, sem er af þóleiít gerð. Granat sést vel í berginu, þ.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|||0.9|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|||||||||||||||
H-173|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - 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|||10.0|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|||||||||||||||
H-174|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|375079|436063|-21.76236|64.16189|14||Basaltgangur, fínkorna 50 - 80 cm þykkur. 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|||5.7|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|||||||||||||||
H-175|Guðmundsson et al., 1995|Sigurðsson et al., 2000|17.9.1993|Surface|Hvalfjörður - Ferstikla, below the farm belonging to Vífil Búason|375087|436059|-21.59102|64.40347|13||Basaltgangur, fínkorna þóleiít 0,5 m þykkt, vestan við líparítganginn. Virðist eitthvað ferskari, en ekki sést hvor líparítgangurinn skeri basaltið eður 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|||0.6|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|||||||||||||||
HG-1|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393077|392359|-21.18684|64.01786|83||Móberg við Sauðá, nokkuð innan við bæinn Gufudal, dökkbrúnt með grænleitum yrjum, í smektít belti.|Tuff rock by Sauðá, somewhat inside the town of Gufudalur.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.59|Measured on crushed sample by Western Atlas Borehole Laboratories|21.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.6|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|||||||||||||||
HG-2|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393118|392463|-21.18608|64.01880|89||Þétt þóleiít 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|0.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|||||||||||||||||||||||
HG-3|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393124|392524|-21.18600|64.01935|93||Ljósgrágrænt móbergstúff, etv í blandlagi, en innan smektít-beltis, við jarðhitasprungu, ca 50 m innan við HG-2, við 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|37.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|37.1|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|||||||||||||||
HG-4|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393144|392580|-21.18563|64.01985|95||Þétt fínkorna þóleiít hraun næst fyrir ofna HG-3, ca. 15-20 cm frá jarðhitasprungunni (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|2.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.3|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
HG-5|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393205|392668|-21.18445|64.02066|112||Móberg í blandlags-belti nokkru innar. Erfitt var að 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|30.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|29.7|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|||||||||||||||
HG-6|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393208|392671|-21.18440|64.02070|113||Laggangur, blöðróttur, holufylltur, 30 cm breiður.  Við 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|9.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|8.7|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|||||||||||||||
HG-7|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393220|392683|-21.18416|64.02081|116||Svipaður laggangur og HG-6, en 10-15 cm breiður. |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|15.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.2|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|||||||||||||||
HG-8|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393335|392762|-21.18187|64.02155|123||Ennþá ofar með Sauðá, móberg í blandlags klórít-belti, á sama stað og Góf og Peter Schiffman tóku sýni H-7 skömmu áður. |Still higher above Sauðá, 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|23.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|22.9|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|||||||||||||||
HG-9|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|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|12.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.5|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
HG-10|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|93371|392819|-27.27359|63.79955|-1206||Þétt þóleít 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|2.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|1.7|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
HG-11|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393417|392907|-21.18029|64.02287|131||Móbergssýni úr bjargi borið niður að Sauðá með framhlaupi úr Reykjafjalli. |Tuff sample from a rock carried down to Sauðá with a run-off from Reykjafjall.|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.74|Measured on crushed sample by Western Atlas Borehole Laboratories|36.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|35.5|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|||||||||||||||
HG-12|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|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|39.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|37.3|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|||||||||||||||
HG-13|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393434|392930|-21.17996|64.02308|132||Áberandi grófkorna, gjallríkt móbergstúff eða þursi úr framhlaupsbjargi. Sýni HG-11-13 eru eingöngu palagónítiseruð en ekki jarðhitaummynduð.|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|36.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|35.4|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|||||||||||||||
HG-14|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393467|392973|-21.17931|64.02348|135||Þétt þóleítbasalt úr stuðluðum hluta hrauns, sambærilegt við 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|0.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.1|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
HG-15|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393463|392996|-21.17940|64.02368|140||Basaltgangur (N-S/90, 40 cm) í Grensdalsmyndun við Sauðá í kl-belti.  Sama og sýni H-9 og H-10 hjá Schifman. |Basalt dyke (N-S / 90, 40 cm) in Grensdalsmyndun by Sauðá 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|15.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.4|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|||||||||||||||
HG-16|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393469|392995|-21.17928|64.02368|139||Heiðgrænt 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|29.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|29.2|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|||||||||||||||
HG-17|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|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|2.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|0.2|He Gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
HG-18|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Sauðá in the town of Gufudalur in Hveragerði|393509|393119|-21.17856|64.02480|162||Heiðgrænt móberg ofar við Sauðá þar sem við Schifaman tókum sýni H-12 og HV-1-3, í klórítbelti. |Green tuff above Sauðá, 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|32.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|31.6|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|||||||||||||||
R-1|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kaldársel í Hjallamisgenginu|360637|394493|-21.85150|64.02539|101||Fínkorna hraun við Kaldársel í Hjallamisgenginu.  Sýni R-1 er ca 5 m neðan við efri brún helluhraunsins í þéttasta hluta þess sem er með óreglulegar þverrákir (einskonar stuðlar), en hraunið er auk þess stórstuðlað þar sem hver stuðull er um 1 m í þvermál.|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|6.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|6.4|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|||||||||||||||
R-2|Sigurðsson and Stefánsson, 1994|Guðmundsson 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 blöðróttari 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|13.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|12.5|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|||||||||||||||
R-3|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|29.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|28.6|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)|||||||||||||||
R-4|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|41.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|39.6|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)|||||||||||||||
R-5|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360688|394460|-21.85043|64.02511|103||Næsta hraun ofan við R-1 til R-4.  Borað var niður í helluhraunsfleka, mjög blöðróttan. |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|39.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|39.2|He gas pycnometry, Geological Survey of Denmark|||||1.13E-11|Measured by Western Atlas Borehole Laboratories|||||||||||||||
R-6|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360676|394446|-21.85043|64.02511|103||Næsta hraun ofan við R-1 til R-4.  Borað var niður í helluhraunsfleka, mjög blöðróttan. |Same as R-5.|Lava flow|Flow-top breccia|Unaltered|3.03|Measured on crushed sample by Western Atlas Borehole Laboratories|||36.7|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)|||||||||||||||
R-7|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Reykjanes peninsula, Kaldársel on the Hjallamisgengur|360676|394446|-21.85066|64.02498|103||Rauðamalargjall úr bruna í vegi við Hjallamisgengið. Flokkað 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|||||||||||||||||||||||||||
R-8|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Reykjanes peninsula, between Valahnúkur and Helgafell|361274|393514|-21.83759|64.01688|137||Jökulbergsset úr móbergi og hálfrúnuðum 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|28.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|25.3|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|||||||||||||||
R-9|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Valahnúkar|361388|393629|-21.83535|64.01795|146||Þursamóberg úr Valahnúkum, brúnleitt með 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|25.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|23.6|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)|||||||||||||||
R-10|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Helgafell|361367|393347|-21.83553|64.01541|142||Móbergstúff úr Helgafelli, norðaustantil.|Tuff rock from Helgafell, northeast.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.70|Measured on crushed sample by Western Atlas Borehole Laboratories|48.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|45.6|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|||||||||||||||
R-11|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|East of Helgafell and Valahnúkar|361439|393461|-21.83416|64.01647|145||Hraun austan við Helgafell og Valahnúka, tekið í misgengisstalli.  Þetta sýni er ca 3 m neðan yfriborðs, borað á ská niður.|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|14.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|13.9|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|||||||||||||||
R-12|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|East of Helgafell and Valahnúkar|361454|393465|-21.83387|64.01650|146||Er úr sama hrauni tekið á yfirborði, lóðrétt niður 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|31.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|31.0|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|||||||||||||||
R-13|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Helgafell|361128|392916|-21.84001|64.01146|229||Móbergstúff úr austanverðu 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|46.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|45.6|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|||||||||||||||
R-14|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Helgafell|361142|392923|-21.83973|64.01153|225||Sama móbergstúff og R-13 en úr grófkorna lagi, sem virðist 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|49.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|47.6|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|||||||||||||||
R-15|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|38.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|38.4|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)|||||||||||||||
R-16|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|46.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|45.3|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|||||||||||||||
R-17|Sigurðsson and Stefánsson, 1994|Guðmundsson 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|39.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|39.4|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|||||||||||||||
R-18|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn|353975|385666|-21.97910|63.94355|228||Kleifarvatn, við veg norðan til. Þetta sýni er úr bólstrabroti í þursabergbreksíu sem er ekki ýkja palagóníseruð. Af þeim sökum tókst ekki að ná sýni úr túffhlutanum nema úr því 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|27.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|27.4|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|||||||||||||||
R-19|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn|353978|385664|-21.97905|63.94352|227||Fínkornótt túff, sama stað 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|45.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|44.2|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|||||||||||||||
R-20|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352310|382178|-22.00964|63.91159|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|23.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|23.5|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|||||||||||||||
R-21|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352309|382184|-22.00966|63.91164|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|25.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|25.2|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|||||||||||||||
R-22|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352308|382190|-22.00968|63.91169|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|31.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|31.7|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|||||||||||||||
R-23|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352308|382197|-22.00969|63.91176|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|30.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|29.8|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|||||||||||||||
R-24|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352310|382206|-22.00967|63.91183|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|30.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|29.7|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|||||||||||||||
R-25|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Kleifarvatn úr syðsta tanganum|352312|382214|-22.00964|63.91191|135||Kleifarvatn úr syðsta tanganum (Lambhaga).  Þar er fallegt ólivín þóleiít bólstraberg í fjörunni austast. Bólstranir eru fremur smáir, þvermál ca 30-40 cm, óreglulega stuðlaðir. Fjögur sýni eru boruð frá glerkápu inn í bólstrana, en tvö í þétta innviði.|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|24.1|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|24.0|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|||||||||||||||
R-26|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Syðrihöfði|353108|383759|-21.99492|63.92609|150||Syðrihöfði.  Fínkornótt túff, borað 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|40.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|40.0|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|||||||||||||||
R-27|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Syðrihöfði|353113|383757|-21.99482|63.92608|150||Syðrihöfði.  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|42.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|41.5|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|||||||||||||||
R-28|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Syðrihöfði|353114|383736|-21.99478|63.92589|150||Syðrihöfði.  Þursaberg, borað í matrixu. |Syðrihöfði. Agglomerate breccia, drilled into the fine matrix.|Hyaloclastite|Hyaloclastite breccia|Unaltered|2.79|Measured on crushed sample by Western Atlas Borehole Laboratories|28.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|28.20|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|||||||||||||||
R-29|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995||Surface|Syðrihöfði|353104|383733|-21.99498|63.92585|150||Syðrihöfði.  Bólstrabrot í sama þursabergi og R-28.|Syðrihöfði. 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|19.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.78|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)|||||||||||||||
R-32|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|357604|406364|-21.92469|64.13052|35|||Samples R-32 to R-134 are derived from a single outcrop in the Öskuhlið 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|||12.16|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|||||||||||||||
R-33|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.80|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|||||||||||||||
R-34|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.70|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|||||||||||||||
R-35|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.90|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|||||||||||||||
R-36|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.59|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|||||||||||||||
R-37|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.32|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|||||||||||||||
R-38|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.32|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|||||||||||||||
R-39|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.30|He gas pycnometry, Geological Survey of Denmark|||||5.00E-16||||||||||||||||
R-40|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.13|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|4.10|1.7|||96.0||
R-41|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.32|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|||||||||||||||
R-42|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.83|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|||||||||||||||
R-43|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.25|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|||||||||||||||
R-44|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.44|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|||||||||||||||
R-45|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.02|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|||||||||||||||
R-46|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.14|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|||||||||||||||
R-47|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.55|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|||||||||||||||
R-52|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|||||||||||||||||||||||||||
R-53|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|357604|406364|-21.92469|64.13052|35|||See description for R-32.|Lava flow|Medium-coarse grained basaltic lava|Unaltered|||||||||||||||||||||||||||
R-54|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||32.74|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|||||||||||||||
R-55|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||34.55|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|||||||||||||||
R-56|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||26.66|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|||||||||||||||
R-57|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||36.33|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|||||||||||||||
R-58|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||26.66|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|||||||||||||||
R-63|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||15.97|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|||||||||||||||
R-64|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||14.10|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|||||||||||||||
R-65|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||15.78|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|||||||||||||||
R-66|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.61|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|||||||||||||||
R-67|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||15.38|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|||||||||||||||
R-68|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||16.11|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|||||||||||||||
R-69|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||16.55|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|||||||||||||||
R-70|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||14.56|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||||||||3.85|4.20|1.7|||57.0||
R-71|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||17.63|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|||||||||||||||
R-72|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||14.93|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|||||||||||||||
R-73|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||15.05|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|||||||||||||||
R-74|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||15.32|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|||||||||||||||
R-76|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.84|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|||||||||||||||
R-77|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.81|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|||||||||||||||
R-78|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||33.45|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|||||||||||||||
R-79|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.91|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|||||||||||||||
R-80|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||34.11|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|||||||||||||||
R-81|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||32.63|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|||||||||||||||
R-82|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||27.28|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|||||||||||||||
R-83|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||36.34|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|||||||||||||||
R-85|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||28.66|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|||||||||||||||
R-88|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||29.71|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|||||||||||||||
R-90|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.61|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|||||||||||||||
R-91|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||26.35|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|||||||||||||||
R-92|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||31.35|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|||||||||||||||
R-93|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||29.91|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|||||||||||||||
R-94|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||31.75|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|||||||||||||||
R-95|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||28.94|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|||||||||||||||
R-96|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||29.32|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|||||||||||||||
R-97|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||31.16|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|||||||||||||||
R-98|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||33.30|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|||||||||||||||
R-100|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||31.38|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||
R-101|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||29.52|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|||||||||||||||
R-102|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.33|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|||||||||||||||
R-103|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.99|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|||||||||||||||
R-104|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||27.40|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|||||||||||||||
R-105|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||30.48|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|||||||||||||||
R-106|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||31.74|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|||||||||||||||
R-107|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.03|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|||||||||||||||
R-108|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.66|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|||||||||||||||
R-110|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.90|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|4.10|1.6|||112.0||
R-111|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.14|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|||||||||||||||
R-112|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||10.99|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|||||||||||||||
R-113|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.95|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|||||||||||||||
R-114|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.32|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|||||||||||||||
R-115|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.10|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|||||||||||||||
R-116|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.31|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|||||||||||||||
R-117|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.70|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|||||||||||||||
R-118|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.36|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|||||||||||||||
R-119|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.78|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|||||||||||||||
R-123|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||13.31|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|||||||||||||||
R-124|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.96|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||
R-125|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.59|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|||||||||||||||
R-126|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.53|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|||||||||||||||
R-127|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.10|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|||||||||||||||
R-128|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||11.63|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|||||||||||||||
R-129|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||12.46|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|||||||||||||||
R-130|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||23.28|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|||||||||||||||
R-131|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||24.95|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||||||||3.75||4.35|2.05||60.0||
R-132|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||24.39|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|||||||||||||||
R-133|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||22.37|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|||||||||||||||
R-134|Friðleifsson & Vilmundardóttir, 1998|||Surface|Reykjavík - Öskuhlíð|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|||26.38|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|||||||||||||||
S-1|Guðmundsson et al., 1995|Sigurðsson et al., 2000|20.9.1993|Surface|Lýsuhóll, Snæfellsbær|299929|489362|-23.22000|64.84465|51||Kjarni úr botni gryfju á útfellingasvæðinu á Lýsuhóli rétt norðan við 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|||47.74|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|||||||||||||||
S-2|Guðmundsson et al., 1995|Sigurðsson et al., 2000|20.9.1993|Surface|Lýsuhóll, Snæfellsbær|299935|489362|-23.21987|64.84466|50||Tekið á sama stað nema í toppinum á kísilbreiðunni. |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|||45.82|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|||||||||||||||
S-3|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300802|490195|-23.20280|64.85263|222||Granófýr tekinn á hæð ofan við 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|||6.81|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|||||||||||||||
S-4|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|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|||0.50|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|||||||||||||||
S-5|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300803|490414|-23.20309|64.85459|264||Úr granófýr við gabbrókontakt. Granófýrinn er grófkorna við kontaktinn. Dökka bergið við kontaktinn virðist vera blanda. E.t.v. Er það blandberg af gabbróinu (glerkennt og dökkt) og því súra (ljósara)? Það 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|||6.58|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|||||||||||||||
S-7|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300855|490498|-23.20211|64.85538|301||Gabbró ofarlega í gilinu vestan við ána, ca. 50 m ofan við 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|||4.20|He gas pycnometry, Geological Survey of Denmark|||||||||||||||||||||
S-8|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300797|490550|-23.20340|64.85581|293||Á sama stað og S-7. Virðist 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|||5.97|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|||||||||||||||
S-9|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300797|490550|-23.20340|64.85581|293||Sami steinn og S-8 og tekið úr dekkri og fínkornaðri hluta steinsins. Fínkornaðri 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|||2.78|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|||||||||||||||
S-10|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300570|489959|-23.20735|64.85038|140||Granófýr eða rhyolít úr skriðu ofan við S-9 upp í hlíðinni vestan í skarðinu. |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|||6.29|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|||||||||||||||
S-11|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300570|489959|-23.20735|64.85038|140||Granófýr eða rhyolít úr skriðu ofan við S-9 upp í hlíðinni vestan í skarðinu. |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|||5.07|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|||||||||||||||
S-12|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300570|489959|-23.20735|64.85038|140||Neðarlega í Lýsuskarði, tekið úr 0.5-1 m þykkum keilugangi, strik 13° halli 30°A.|At the bottom of Lýsuskarð, 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|||0.39|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|||||||||||||||
S-13|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300556|489958|-23.20764|64.85036|136||Hraunlag neðan við keiluganginn (S-12), blöðrótt 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|||0.41|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|||||||||||||||
S-14|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300556|489958|-23.20764|64.85036|136||Tekið úr sama lagi og S-13, nema bergið virðist blöðróttara, 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|||1.05|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|||||||||||||||
S-15|Guðmundsson et al., 1995|Sigurðsson et al., 2000|21.9.1993|Surface|Lýsuhóll, Snæfellsbær|300494|489806|-23.20874|64.84897|101||Rétt ofan við neðsta foss í gilinu. Tekið úr keilugangi sem sker granófýrinn í S-16. Bergið 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|||3.62|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|||||||||||||||
S-17|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|291475|487904|-23.39561|64.82644|6||Búðarhraun, úr stálinu (þétta 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|||9.49|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|||||||||||||||
S-18|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|291483|487898|-23.39543|64.82639|6||Búðahraun- úr frauðkennda 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|||17.03|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|||||||||||||||
S-19|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|278009|483833|-23.67213|64.78136|253||Basaltrík breksía við Stapafell við 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|||17.75|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|||||||||||||||
S-20|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|278045|483833|-23.67139|64.78138|257||Sami staður og S-19. Tekið úr bólstraða 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|||10.35|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|||||||||||||||
S-21|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|277808|494474|-23.69296|64.87642|199||Jökulberg (set) Norðan við Snæfellsjökul á leið niður. Bergið vel samlímt.|Tillite north of Snæfellsjökull 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|||17.76|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|||||||||||||||
S-22|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|277756|494402|-23.69393|64.87574|205||Rauðleitt jökulsbergsset tekið rétt ofan við 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|||19.64|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)|||||||||||||||
S-23|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|277792|494472|-23.69328|64.87639|200||Stórstuðlað bólstra eða 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|||0.75|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|||||||||||||||
S-24|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Snæfellsbær|278593|495350|-23.67780|64.88478|102||Stuðlað berg líklega eldri grágrýtismyndun skammt ofan við Ólafsvík. Gæti verið 30 m þykkt. 20 m af stuðlum og 10 m af kubbabergi. Bergið er fínkorna og grátt að 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|||5.08|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|||||||||||||||
S-25|Guðmundsson et al., 1995|Sigurðsson et al., 2000|22.9.1993|Surface|Grundarfjarðarbær|310316|500170|-23.01597|64.94746|21||Kolgrafarfjörður/Hraunsfjörður. Grófkorna gabbró, grænleitt vegna ummyndunnar. Sýni tekið við veg, þar sem beygt er inn í Hraunfjörð. |Kolgrafarfjörður/Hraunsfjörður. Coarse-grained basalt, green-colored due to alteration. Sample taken where the road turns into Hraunsfjörður. |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|||1.76|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|||||||||||||||
S-26|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|286613|491258|-23.50280|64.85339|327||Bólstrabergs.- kubbabergsmyndun frá jökulbergsmyndun. Sýnið er tekið úr þéttum 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|||8.73|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|||||||||||||||
S-27|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|286613|491258|-23.50280|64.85339|327||Bólstraberg. Sama myndun og S-26 nema sýni tekið inn á milli bólstra, mun meira sprungið.|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|||7.31|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|||||||||||||||
S-28|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|286613|491258|-23.50280|64.85339|327||Basalthraun. Líklega úr sömu myndun og S-26 og 27. Stór veruleg stuðlun 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|||6.73|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|||||||||||||||
S-29|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|286613|491258|-23.50280|64.85339|327||Móberg. Líklega sama myndun og S-26 - 28. Eins konar móbergshroði. Sýnatökustaður um 200 m ofan við sæluhúsið á Fróðárheiði.|Tuff. Probably the same formation as S-26-28. A kind of tuff. Sampling point about 200 m above the mountain hut at Fróðárheiði.|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|||33.87|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|||||||||||||||
S-30|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|283383|493117|-23.57355|64.86794|261||Lagskipt túff. Ath. sýni 30-33 öll úr sömu myndun, sýnin tekin innan 10 m2. Bergið virðist 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|||26.65|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|||||||||||||||
S-31|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|283383|493117|-23.57355|64.86794|261||Blóðrauður móbergshroði.|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|||27.08|He gas pycnometry, Geological Survey of Denmark|||||||||||||||||||||
S-32|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|283383|493117|-23.57355|64.86794|261||Basalthraun. Sýni tekið úr vel kristölluðum stuðli um 30 cm breiðum.|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|||5.57|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|||||||||||||||
S-33|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Fróðárheiði, Snæfellsness|283383|493117|-23.57355|64.86794|261||Bólstraberg. Sýni tekið úr ca. 10 cm stuðli.|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|||7.17|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)|||||||||||||||
S-34|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Búlandshöfði, Grundarfjörður|287906|501466|-23.49087|64.94554|92||Basalthraun. Meðal-grófkorna ólivín-þóleiítbasalt e.t.v. Í tertíera hluta Búlandshöfða, áberandi kúluveðrun. Sýni tekið við veginn í ca. 60 m hæð. |Basalt lava. Medium-coarse-grained olivine-tholeiite basalt. Perhaps in the tertiary part of Búlandshöfði, 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|||7.12|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|||||||||||||||
S-35|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Grundarfjarðarbær|304343|499577|-23.14125|64.93870|7||Basalthraun. Tertíert fínkorna þóleiíthraun með 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|||1.34|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|||||||||||||||
S-36|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|304232|499812|-23.14393|64.94074|1||Andesít. Fín - dulkorna andesítgangur. Sýni tekið í Eiðisstapa, þann er Landstapi heitir, sunnan við Sjóstapa.|Fine-grained, andesite dyke. Samples taken in Eiðisstapi, 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|||0.70|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|||||||||||||||
S-37|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|303754|497146|-23.15031|64.91659|199||Hraunlag. Meðalkorna ólivín-þóleiítbasalt, líklega um 8 m þykkt. Sýni tekið úr gili ofan við æfingasvæði 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|||1.09|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|||||||||||||||
S-38|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|303789|497141|-23.14956|64.91657|188||Súrt innskot. Sýni tekið úr stuðlupu blöðróttu bergi. Stuðlar um 25 cm breiðir. 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|||12.35|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|||||||||||||||
S-39|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|303809|497141|-23.14915|64.91658|183||Súrt berg. Sýni tekið úr eins konar blandbergi og var þetta 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|||0.64|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|||||||||||||||
S-40|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|303809|497141|-23.14915|64.91658|183||Basalt. Sama berg og S-39 og nú tekið 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|||1.42|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|||||||||||||||
S-41|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|305545|495987|-23.11095|64.90727|198||Basalthraun. Grófkorna ólivín-þóleiítbasalt. Ofarlega í því er 0,5 - 1 m þykkur 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|||5.00|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|||||||||||||||
S-42|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|306578|500532|-23.09539|64.94856|20||Ísúrt berg. Ísúr keilugangur í gabbrói við 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|||0.35|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|||||||||||||||
S-43|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|306882|501300|-23.09003|64.95560|18||Gabbró. Sýni tekið við vegkannt, grófkorna og grænleitt 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|||0.71|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|||||||||||||||
S-44|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|306988|501339|-23.08785|64.95601|20||Gabbró. Sýni tekið við vegkannt um 20 m NA við S-43. Steinarnir eru ættaðir úr klettum beint fyrir ofan sýnatökustaðina. |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|||1.70|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|||||||||||||||
S-45|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|306974|501367|-23.08818|64.95626|15||Gabbró, tekið á sama stað 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|||0.96|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|||||||||||||||
S-46|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|306974|501367|-23.08818|64.95626|15||Gabbró, tekið á sama stað 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|||1.10|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|||||||||||||||
S-47|Guðmundsson et al., 1995|Sigurðsson et al., 2000|23.9.1993|Surface|Kolgrafir í Eyrarsveit, Grundarfjörður|307007|501460|-23.08760|64.95711|9||Gabbró, mjög grófkorna og er ca. 100 m austan við S-46 við 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|||1.14|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|||||||||||||||
E-13|Guðmundsson et al., 1995|Sigurðsson et al., 2000|27.8.1993|Surface|Reykjavik|363325|421973|-21.82166|64.27272|94||Gangberg. 2 m þykkur meðalkorna þóleiítgangur. Sýni tekið u.þ.b. úr miðjum ganginum, sem er í gilinu ofan við 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|||6.80|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)|||||||||||||||
E-28|Guðmundsson et al., 1995|Sigurðsson et al., 2000|6.9.1993|Surface|Mosfellsbær|376333|414227|-21.54697|64.20826|153||Dólerít? veðrunarútlínur eins og í ólivínþóleiíti, bergið virtist gjallkennt og blöðrótt. Lagið liggur í hlíðinni miðri eða rétt ofan við skriðu. |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|||10.78|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)|||||||||||||||
E-31|Guðmundsson et al., 1995|Sigurðsson et al., 2000|6.9.1993|Surface|Mosfellsbær|376346|414234|-21.54672|64.20832|153||Fínkorna innskot (silla) um það bil 4 m ofan við E-30 (Dólerítið? 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|||||||||||||||||||||||||||
EÞ-3|Guðmundsson et al., 1995|Sigurðsson et al., 2000|26.8.1993|Surface|Reykjavik|366676|414856|-21.74618|64.21026|54||Dólerít innskot. Í stórum steini um 2 m frá EÞ-1 og EÞ-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|||0.35|He gas pycnometry, Western Atlas Borehole Laboratories (2 measurements) and Geological Survey of Denmark (2 measurements)|||||||||||||||||||||
KH-3|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð 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|26.9|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|25.30|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|||||||||||||||
KH-4|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|45|Dýpi 44.95-45.10 m, Halarauður.|Halarauður (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|12.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|12.40|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|||||||||||||||
KH-5|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|47|Dýpi 46.75-46.9 m, Halarauður úr kassa 4 (rauð og svört sambreiskja).|Halarauður 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|16.5|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|16.40|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|||||||||||||||
KH-6|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|49|Dýpi 48.95-49.10, Halarauður - gráleitur með rauðum molum í en ekki sambrædd eða með slíkum strúktúr heldur eins og breksían sé samlímd og hafi ekki runnið til.|Halarauður - 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|21.6|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|21.30|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|||||||||||||||
KH-7|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|54|Dýpi 54.13-54.23. Neðan við Halarauð. Grásvört samlímd (líklega með zeólítum) breksía.|Below Halarauður. 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|15.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.70|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|||||||||||||||
KH-8|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð 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|16.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|16.00|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|||||||||||||||
KH-9|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|64|Dýpi 63.9-64.0 m, blöðrótt grátt basalt og það 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|17.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.20|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|||||||||||||||
KH-10|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|69|Dýpi 68.5-68.6 m, fínkornótt smásprungið basalt og hálf blöðrufyllt.|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|21.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|21.60|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|||||||||||||||
KH-11|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð 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|32.7|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|31.90|He gas pycnometry, Western Atlas Borehole Laboratories|||||||||||||||||||||
KH-12|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð 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|13.2|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|12.05|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|||||||||||||||
KH-13|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|94|Dýpi 94.3-94.4 m, Basaltbreksía milli hraunlaga og er ljósgræn 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|11.3|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|11.30|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|||||||||||||||
KH-14|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|115|Dýpi 115.2-115.3 m, sæmilega - illa kristallað fín-meðalkorna 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|18.4|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.60|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|||||||||||||||
KH-15|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|127|Dýpi 127.33-127.43 m, fínkornótt blöðrótt 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|11.8|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|11.70|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|||||||||||||||
KH-16|Sigurðsson and Stefánsson, 1994|Guðmundsson et al., 1995|26.2.1993|Borehole|Sandabotnaskarð hole KH-1 - Krafla|604229|577882|-16.73214|65.70167|606|131|Dýpi 131.2 - 131.3, samþjappað móberg eða 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|19.0|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.40|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|||||||||||||||
ÖJ-1-1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|795|Hlutkristallað móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|||||||||||||||||||||||||||
ÖJ-1-2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|795|Meðalögrófkorna mjög ummyndað og eða blöðrótt basalt|Medium-grained highly altered and/or vesicular basalt|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|||||||||||||||||||||||||||
ÖJ-1-5|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallað móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|||||||||||||||||||||||||||
ÖJ-1-6.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallað 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"||||||||
ÖJ-1-6.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallað 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|14.87|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|14.60|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"||||||||
ÖJ-1-7|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallað móberg|Partially crystalline tuff|Hyaloclastite|Hyaloclastite tuff|Chlorite-epidote|||||||||||||||||||||||||||
ÖJ-1-7.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|796|Hlutkristallað 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|14.75|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|14.85|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"||3.63||2.08|0.3||27.0|10.8
ÖJ-1-7.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|14.29|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|13.60|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"||||||||
ÖJ-1-8.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|16.05|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.03|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"||||||||
ÖJ-1-9.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|16.38|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|16.14|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"||3.67||2.12|0.3||27.9|11.2
ÖJ-1-10.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|16.27|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|15.48|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"||||||||
ÖJ-1-10.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|17.64|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|17.46|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"||||||||
ÖJ-1-11.1|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|797|Hlutkristallað 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|18.89|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|18.48|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"||||||||
ÖJ-1-11.2|Franzson & Tulinius, 1999||24.2.1995|Borehole|Ökelduháls ÖJ-1, near Nesjavellir|390146|396973|-21.25010|64.07702|287|798|Hlutkristallað 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|20.44|Determined from volume measurements in Hg on crushed sample, i.e. (bulk volume - grain volume) / bulk volume|19.73|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"||||||||
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 samsíða 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|||43.10|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).||||||||1.50|2.34||||15.0||
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 samsíða 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|||37.60|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).||||||||1.95|||||14.0||
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|||42.60|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).||||||||1.45|1.90||||12.9||
150803-05|Franzson et al., 2011|Frolova et al., 2005|15.8.2003|Surface|Votuklettar-Threngsli|380188|387680|-21.44651|63.99035|333||"Skriðukennt ""foreset"" lagskipting, halli 25° og strikstefna 351°. Kornastærð <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|||15.70|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).||||||||2.30|4.30||||79.0||
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. Kornastærð <0,5cm. Kjarni þvert 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|||29.80|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).||||||||1.30|||||||
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 þykk lög. Kjarni þvert 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|||34.30|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).||||||||2.50|2.85||||37.0||
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 yfirborði inn í neðri 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|||30.30|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).||||||||1.95|2.65||||43.0||
170803-01|Franzson et al., 2011|Frolova et al., 2005|17.8.2003|Surface|Stora Dímon|405170|414657|-20.95377|64.23387|390||Suðurhlíðar 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|||37.90|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).||||||||0.90|1.15||||2.2||
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|||40.30|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).||||||||1.05|1.50||||1.8||
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 suðurs, tuff lagst til ofan vatnsborðs og nærri gígnum. Efsti hluti kjarnans oxideraður, sem hverfur um 2-3 cm neðar. |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|||53.30|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).||||||||1.55|||||3.1||
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 stærri túffmola (t.d. Sýni 3). Prímert túff með 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|||42.30|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).||||||||1.05|1.70||||2.8||
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 tekið 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|||49.80|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).||||||||1.10|1.65||||4.8||
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 neðan Yngri Skefilsfjallsmyndun, um 5 m frá bólstrabergs ""innskoti"". Lagskiptingin hallar um 6-7°. Eitthvað uppbrot í túffinu. Túffið er dökkbrúnt efst en verður dekkra er neðar kemur í kjarnanum. Sýni tekið 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|||43.90|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).||||||||1.70|2.10||||9.3||
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, aðeins grófara en sýni 38, (kornastærð 5-1 cm. Yfirborðsoxun hverfandi. Lagskiptin 1-3 m þykk. Kjarni tekin samsíða 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|||42.40|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).||||||||1.65|2.00||||5.1||
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 hærra upp en sýni 17837. setzt til í vatni og rofeinkenni augljós í túffinu. Túffið 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|||39.90|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).||||||||1.85|1.90||||13.0||
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 við lóðréttan jaðar 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|||40.40|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).||||||||1.40|||||5.3||
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 ummynduð 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|||15.10|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).||||||||1.30|3.10||||68.0||
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 við ummyndunina í sýni 10. Bresía sprungin og erfitt að taka heilleg sýni. Breksían líkelgast pr´mer þar 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|||15.30|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).||||||||1.90|4.15||||||
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 þétt túff, dökkt að lit sem líkelgast bendi til aukins magns fersks glers. . Brotgjarnt og sýnataka erfið. |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|||25.40|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).||||||||1.45|3.35||||48.0||
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 við jaðar jarðhitaæðar. 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|||29.30|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).||||||||1.65|2.85||||28.0||
180803-03|Franzson et al., 2011|Frolova et al., 2005|18.8.2003|Surface|Roadcut in Mosfellsbaer|368696|409649|-21.70005|64.16438|63||Ráðandi túff, lagskipting óglögg. Halli laga um 45°NA. Útfellinga fátíðar nema í æðum sjást kabasít og og kalsít.  Brúnleit ummydun við jaðra sprugna, svipað og finnst í sýninu nærri Iðntæknistofnun. |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|||21.60|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).||||||||2.30|3.60||||111.0||
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 frábrugðið túffinu  fyrir ofan og líklegast takmarkað 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|||14.50|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).||||||||1.55|3.15||||41.0||
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 tekið norðan í vegkantinum.  Kjarninn brotgjarn og erfitt að taka sýni. Veðrun áberandi í yzta cm sem gefur vísbendingu um hraða veðrunarinnar.  |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|||23.30|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).||||||||2.40|3.65||||64.0||
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 við veginn. Sýni tekið af 1 cm þykkri ummyndaðri sprungu. |Layered tuff as observed from exposures south of road. Sample taken from a 1 cm thick altered fracture. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite||||||||||||||||||||1.95|2.85||||||
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 tekið samsíða laskiptingu. Lagið er tvískipt. Sýnið tekið um 4 m neðan 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|||26.00|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).||||||||2.95|3.30||||63.0||
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 neðan við dólerítið. Lagskipting í túffinu <5cm. Möguleg misleitni milli sýna, svo velja þarf með varúð.|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|||23.10|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).||||||||4.05|3.75||||99.0||
190803-03|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Meðalfell in Baejargil. |374698|426781|-21.59120|64.32017|169||Lagskipt túff á milli hraunlaga, rúnnun korna sést ekki, en afar líklegt að lagið sé setlag. Kornastærð <1cm, svo búast má við misleitni. Lagið amk. 1 m að þykkt. Lagið er mun fínkornaðra í neðri 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|||26.80|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).||||||||2.10|3.20||||||
190803-04|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Meðalfell in Baejargil. |374751|426882|-21.59019|64.32110|211||6-8 m þykkt túfflag, gróf lagskipting og bóstrabeg í efri hlutanum, en eitt samtíma lag. Verður 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||||||||||||||||||||2.10|||||31.0||
190803-05|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Meðalfell 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|||23.40|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).||||||||3.20|2.90||||48.0||
190803-06|Franzson et al., 2011|Frolova et al., 2005|19.8.2003|Surface|South side of Meðalfell in Baejargil. |374755|426860|-21.59009|64.32090|207||Sýni tekin um 1-15 m neðan við efra borð á 2-3 m þykku settúffi. Lárétt lagskipting, setzt til í vatni, en engin skálaga setstrúktúr sést. Ljósbrúnt að 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|||33.60|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).||||||||2.20|2.05||||||
200803-01|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Miðfell|400998|411911|-21.03784|64.19551|152||Vestan við Thingvallavatn. Skálaga túffset blandað bólstrum og breksíu. Halli laga um 32°og strik 30°.  Kornastærð <1cm, misleitni moguleg. Samlíming takmörkuð svo útlínur kjarnans nokkuð 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|||33.40|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).||||||||1.65|2.25||||2.6||
200803-02|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399739|414901|-21.06575|64.22195|189||Lítið lagskipt túff. Basaltmolar í túffinu upp í 5 cm.  Túffið 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|||38.00|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).||||||||1.30|2.05||||7.6||
200803-03|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399813|415069|-21.06434|64.22348|216|| skolvatnið frá boruninni fremur oxað fyrsta cm sem er vísbendingu um yfirborðsveðrunina. |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|||39.00|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).||||||||1.15|1.70||||6.1||
200803-04|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|Arnarfell. |399677|415100|-21.06716|64.22372|201||Nærri toppi myndunarinnar. Lagskil halla um 10-20°, lagskil ekki samfelld, sem bendir til að lagið hafi orðið til ofan vatnsborðs. Kornastærð <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|||34.60|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).||||||||1.70|2.20||||3.5||
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 tekið. Kjarni samsíða lagskiptingu. Þar nærri er óreglulegur samtíma gangur, en ekki ber á aukningu á palagonitiserungu  nærri ganginum. Sýnataka erfið 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|||44.70|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).||||||||1.70|2.05||||9.5||
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 við jaðar á Reyðarbarmi-Kálfstinds móbergshrygg. Túffið fínkorna og vel samlímt. Kjarnar boraðir samsíða lagskiptingu. |A tuff sequence on the outside of Reyðarbarmur 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|||36.70|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).||||||||1.60|2.10||||12.0||
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. Borað samsíða 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|||46.30|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).||||||||1.50|||||20.0||
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. Borað samsíða 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|||45.50|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).||||||||1.70|1.85||||5.3||
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, borað þvert á lagskiptingu. Kjarni vill springa, líklega vegna bólstrainnskota fyrir neðan.|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|||44.80|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).||||||||1.30|2.10||||9.7||
200803-10|Franzson et al., 2011|Frolova et al., 2005|20.8.2003|Surface|South of Laugardalshellir|408369|413822|-20.88739|64.21470|246||Þykka lagið í staflanum, erfitt að ná heillegum sýnum vegna takmarkaðrar samlímingar. Handsýni tekið líka. Lagið er um 12 m þykkt með 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|||46.10|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).||||||||1.30|||||||
210803-01|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|South end of Vörðufell|423378|394354|-20.56843|64.04381|77||Neðsta móbergið í Vörðufelli. Setkennt, og að hluta vatnslegið. Skálaga lagskipting sést. Þykkt meira en 10 m. Lagið liggur undir hraunlagi. Virðist minna vatnsborið nærri botni lagsins þar sem vart verður við bólstra breksíutopi lagsins. Kvarts þóleiít.  Basalt laggangur í opnunni.|The lowest hyaloclastite found in Vörðufell. 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|||17.20|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).||||||||1.90|||||||
210803-02|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|South end of Vörðufell|423390|394354|-20.56818|64.04382|77||Sýni tekið úr sama lagi en um 2 m neðar í opnunni. Sýnataka erfið 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|||24.10|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).||||||||1.60|||||||
210803-03|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Reykholt Biskupstungur|430031|408496|-20.43888|64.17205|85||Árset, sandsteinskornastærð, 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|||37.70|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).||||||||1.70|||||||
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 þykkt settúff, fínlagskipt, og nærri sýnatökustað 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|||31.20|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).||||||||1.90|2.45||||||
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 þykkt lagskipt túff, svipað og sýni 04, líklegast setlag.  Vandræði 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|||31.20|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).||||||||1.55|1.80||||10.8||
210803-06|Franzson et al., 2011|Frolova et al., 2005|21.8.2003|Surface|Valahnúkar|460534|404132|-19.81055|64.13778|176||Engin lýsing tiltæk|No description given|Hyaloclastite|Hyaloclastite tuff|Unaltered|2.62|Derived from measured porosity, i.e. sample weight / (bulk volume - pore volume), measured by Orkustofnun|||33.40|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).||||||||2.25|2.75||||||
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 með prímert túff, grófkennd lagskipting sem hallar 20-30°V, að því er virðist  gróf skriða en ekki sést ísbending um tengsl við 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|||34.80|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).||||||||2.15|2.60||||21.0||
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 skálagaðs túffs, kornastærð minni en 0,5 cm, rúnnun korna sjáanleg. Sýni tekið efst í laginu sem er lárétt. Rof flötur neðan við. Sýni tekin samsíða 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|||25.00|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).||||||||2.95|3.30||||40.0||
220803-04|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Túff neðan við síðasta sýni. Laghallo um 40° strikstefna  A. Sýni tekið samsíða lagskiptingu. Kornastærð <1cm. Áhugavert að sjá meiri samlímingu þar sem meiri sprungur er að 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|||34.90|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).||||||||1.85|2.40||||10.0||
220803-05|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Sýni tekið ú ralgi sem hallar um 50° og er fremur grófkorna. Kornastærð <2cm, en að metu mun fínkornaðra. |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|||39.80|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).||||||||1.95|2.50||||12.0||
220803-06|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|473326|397803|-19.54672|64.08224|414||Sami stað og síðasta sýni, en tekið úr mun fínkornaðra túffi, halli 50°A og strik N-S. Þetta er líklegt dæmi um flæðibrotflöt 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|||33.60|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).||||||||2.15|2.80||||19.0||
220803-07|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Valahnúkar|475408|397095|-19.50393|64.07605|535||Sama svæði en sýni tekið í grófari hluta túffsins, u.þ.b. 20 m fjarlægð frá síðasta sýni, þ.e. Innan flæðibrotflatar og svo utan hans. S+ýnið er um 16 m frá sýni 05 og liggur neðan þess. |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|||34.80|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).||||||||2.00|2.55||||10.3||
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 vatnsborðs á gostíma. Hraunflyksur. Halli laga 5-10° í vesturátt. Sýni tekið rétt suðaustan 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|||38.50|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).||||||||1.60|2.05||||13.0||
220803-09|Franzson et al., 2011|Frolova et al., 2005|22.8.2003|Surface|Landmannahellishyaloclastite|480581|395842|-19.39777|64.06514|568||Sýni tekið á norðausturhlið sömu móbergmyndunar og Landmannahellir er í. Grófkennd laskipting sem hallar 40-50° til norðurs. Líklega skálaga skriða 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|||39.70|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).||||||||2.70|2.90||||26.0||
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 fjarlægð. |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|||40.60|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).||||||||2.10|2.50||||13.0||
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 með grófa lagskiptingu  sem hallar um 30° með 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|||43.70|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).||||||||1.60|1.90||||8.9||
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° með 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|||37.40|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).||||||||1.80|1.95||||3.5||
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 . Kornastærð <1cm, virðist 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|||21.10|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).||||||||2.35|3.10||||43.0||
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, nær lárétt túfflag nokkuð 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|||28.10|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).||||||||2.40|2.85||||28.3||
050903-01|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|South end of Þjórsárholt by river|441190|392432|-20.20318|64.03008|132||Um 18 m þykkt túff set. Efri hlutinn er völuberg, en neðri hlutinn fínkornaðra með grófari linsum inn á milli sýni tekið í leirlagi um 1-2 m neðan við grófa lagiðlagið er mislægt við hraunlagið 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|||25.40|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).|||||||||||||||
050903-02|Franzson et al., 2011|Frolova et al., 2005|5.9.2003|Surface|Ca. 1 km east of Gaukshöfði and about 2 m from main road|451712|399404|-19.99018|64.09425|133||rúmlega sex metra þykkt túff árset, með breytilegri kornastærð. Lagið sem sýnið var tekið úr er <1m þykkt og er lárétt og fíkorna. Roflænur sjást í setinu rétt ofan við sýnatökusaðinn. |>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|||45.70|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).|||||||||||||||
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 neðan við bólstraberg, líklegt basalt lag sem tilheyrir þessari myndun. Ferskt gler, palagonít með takmörkuðum 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|||12.20|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).|||||||||||||||
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 , þétt og leirkennt set með molum upp að 40cm. Sýni tekið úr fína hlutanum, lagskipting sést illa. Gæti verið leirflóð. |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|||22.70|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).|||||||||||||||
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 rýþmískt árset. Fínkorna með stærri molum (<5cm) inn á milli. Roflænur sjás innan setsins og rúnnun setkorna. Sýnið tekið innan fínkornaðasta 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|||28.40|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).|||||||||||||||
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 nær 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|||19.70|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).|||||||||||||||
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 tekið 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|||26.90|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).|||||||||||||||
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 með 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|||10.40|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).|||||||||||||||
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 ætti að sjást í þunnsneiðargreiningu. Sýnataka erfið 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|||14.50|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).|||||||||||||||
120903-05|Franzson et al., 2011|Frolova et al., 2005|12.9.2003|Surface|E-Thjorsárdalur|459583|406791|-19.83079|64.16152|160||Tuúff með ógreinilega lagskiptingu, líklega prímer. Fíkorna ´tuff með g´rofari lögum inn á milli. Opnan er um 20 m þykk 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|||23.20|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).|||||||||||||||
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 með 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|||10.30|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).|||||||||||||||
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 nær ólagskipt túff með nokkurri misleitni. Ólivín þóleiite gangur sker túffið og hefur strikstefnu 310°.  Um 4 m þykkt ummyndunarbelti er fram með ganginum berandi vitni um jarðhitaummyndun. Sprungustefnur 30 og 80°. Bólstraberg í grennd. Ummyndunarsteindir kalsít, skólesít og stilbít. kjranataka erfið 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|||9.50|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).|||||||||||||||
291004-01|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarð in Hengill|383694|394600|-21.38030|64.03490|341||Sýni úr ferska hluta túffsins. Ummyndun sjáanleg í túffinu en virðist einskorðast við 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|||26.90|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).|||||||||||||||
291004-02|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarð in Hengill|383695|394610|-21.38029|64.03499|341||Ummynað túff, þótt ekki sjáist til útfellinga. Laghalli um 30Å 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|||46.00|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).|||||||||||||||
291004-03|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarð in Hengill|383692|394622|-21.38036|64.03510|341||Fremur grófkorna túff, lagskipting svipuð 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|||41.90|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).|||||||||||||||
291004-04|Franzson et al., 2011|Frolova et al., 2005|29.10.2004|Surface|Hellisskarð in Hengill|383682|394638|-21.38058|64.03524|338||Dökkgrátt, mjög fínkorna og þétt túff. Þetta túff eru hnullungar um 30 cm í þvermál 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|||37.90|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).|||||||||||||||
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 Arnarþúfu vestur af Vífilfelli. Lítil túffnáma. Túffið er illa lagskipt og líklega prímert. Túffið 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|||35.30|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).|||||||||||||||
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. Sýnið er tekið frá líklegri gosrás túffsins. Laghallinn er <30° og gæti verið ""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|||45.70|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).|||||||||||||||
011104-04|Franzson et al., 2011|Frolova et al., 2005|1.11.2004|Surface|Sandfell in Þrengsli, west side. Slightly north and above the quarry.|379083|386078|-21.46777|63.95693|245||Sýnið tekið innan illa lagskipts túffs, með tiltölulega misleitna kornastærð, og líklegast prímer. Mjög fínlagskipt túff (mögulega þekja af jökulkyni) liggur ofan á túffinu og hallar 30°með strikstefnu 60°. Túffið getur verið þetta týpíska túffþekja 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|||33.50|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).|||||||||||||||
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 að 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|||39.80|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).|||||||||||||||
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 þvert 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|||40.50|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).|||||||||||||||
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 skriðu vinstra meginn við veginn, um 50 m frá, líklegast í norðaustur hluta Tófubruna hrygg. Lagskil óveruleg. Líklegast prímert, og róteraðir  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|||39.20|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).|||||||||||||||
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. Þarf að 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|||36.60|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).|||||||||||||||
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 móbergið til hægri á norðurenda Vigdísarvallavegi. Prímert túff, fremur fínkorna inn á milli grófara túffs. Lagskipting ógreinileg. Móbergshlunkar með 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|||33.40|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).|||||||||||||||
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 pakkað með jökulleir. Borað þvert 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|||22.10|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).|||||||||||||||
021104-03|Franzson et al., 2011|Frolova et al., 2005|2.11.2004|Surface|Vigdísarvellir track|354299|387249|-21.97402|63.95786|210||Sýni tekið þar sem vegurinn sveigir upp brekkuna. Prímert túff. Ógreinieg lagskilsamlíming virðist meiri við 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|||37.70|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).|||||||||||||||
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 tekið nærri vegi lengra til suðausturs. Tékka þarf á misleitni milli kjarna. Fínlagskiptari túff inn á milli (sem oft má sjá í þessari túffgerð. Þessi lög eru oft hreyfð, sem bendir til hreyfingar á túffinu meðan 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|||44.10|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).|||||||||||||||
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 nærri vegi lengra í suðaustur. Líklegast ""skriða í vatni"". Lagþykkt <20 cm. Mætti aðgæta val á kjörnum til samræmis. Nokkur oxun. Lögin halla um 20° og með strikstefnu 50°. Sýni tekið um 20 m ofan vegar og nærri botni 30 m þykks túfflags. skriðueinkenni ekki til staðar, þ.e. að lagið heldur jafnri 10 m þykkt um 10 m. mögulea sama lag og sýni 04 að því undanskyldu að það 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|||32.10|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).|||||||||||||||
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 tekið hornrétt á lagskiptinguna.  Áhugavert að 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|||43.80|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).|||||||||||||||
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 ummyndað ljósleitt túff, allt gler ummyndað, 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|||37.40|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).|||||||||||||||
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 tekið um 100 m norðaustan við veginn.  Prímert túff, sýni frekar misleit og þarf að 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|||49.40|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).|||||||||||||||
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 þar sem það er mest fínkorna. Lagskil hallar um 20° en óreglulega. Túff telst vera prímert en mætti endurskoða, gæti verið 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|||41.20|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).|||||||||||||||
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||Skriðukenndur rofflötur fyrir ofan sýnatökustað þar sem túffið er mun betur lagskipt (ca. 5-6 m) og var sýni tekið þar þar sem þykkt laga er <2cm. Þar fyrir ofan er túffið veður mun grófara og minna lagskipt, sem bendir til aukinnar gosvirkni. Halli laga er um 1°. fjarlægð 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|||40.00|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).|||||||||||||||
031104-04|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Ingólfsfjall quarry|399360|385878|-21.05413|63.96164|180||Sýni tekið um 10 m vestan sýnis 03. Áhugavert að sjá að túffið er lárétt eins og lárétt hraun sem liggja ofan á túffinu bera með 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|||18.10|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).|||||||||||||||
031104-06|Franzson et al., 2011|Frolova et al., 2005|3.11.2004|Surface|Southeast corner of Þingvallavatn|401787|404952|-21.01704|64.13335|102||Móbergsmyndun við suðaustur horn Þingvallavatns. Hallandi lagskil greinanleg. Sýni tekið innan frekar fíngerðs túffs, en grófari breksía þa 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|||28.20|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).|||||||||||||||
HE-01|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|435931|327114|-20.28361|63.44341|29||"Heimaey. Skipahellir. Loftborið túff með bombu gígum og ""accretionary lapilli"".  Utan gígsvæðis. 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|||37.50|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).|||||||||||||||
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|||38.80|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).|||||||||||||||
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 Sæfelli sem er 6000 ára. Surtseyjar gosstíll. Einhver palagonitisering í túffinu. Lögins halla 16°með 60° strikstefnu. |Heimaey. Topp of Sæfell 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|||41.50|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).|||||||||||||||
HE-04|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Heimaey|436491|323073|-20.27077|63.40727|51||Heimaey. Neðsti hluti Sæfells sem er 6000 ára. Mjög palagonitiserað lagskipt túff. Lítt hallandi lagskipting. Palagónitiseringin líklegast vegna jarðhitaflæðis frá gosstöðinni. |Heimaey. Bottom of Sæfell 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|||35.20|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).|||||||||||||||
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 loftborið 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|||34.50|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).|||||||||||||||
SU-05|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Surtsey|419680|311957|-20.60138|63.30418|105||"Surtseyjarðhitasprunga með 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|||46.70|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).|||||||||||||||
Helgafell|Franzson et al., 2011|Frolova et al., 2005|31.12.2004|Surface|Helgafell near Hafnafjörður|547268|495824|-17.99944|64.95919|842||Nær 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|||34.00|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).|||||||||||||||
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|||14.60|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||||||||
3 (KH-24)|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarð|604229|577882|-16.73214|65.70167|606|172|Allt lagið er oxað og blöðrur 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|||2.18|Triple Weight|||||||||0.005|0.078|||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
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|||20.30|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
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|||8.06|Triple Weight|||||||1177|0.0008495|4.01E-02|0.011193687|552||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
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|||19.90|Triple Weight|||||||||8.00E-03||90.6||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
9|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|27.5.1995|Borehole|Krafla KH-2, Sandabotnaskarð|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|||9.70|Triple Weight|||||||288|0.0034760|8.36E-02|0.011165204|227||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
11|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|24.6.1995|Borehole|Krafla KH-3, Sandabotnaskarð|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|||2.24|Triple Weight|||||||||0.150||||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
18|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|24.6.1995|Borehole|Krafla KH-3, Sandabotnaskarð|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|||3.27|Triple Weight|||||||||0.150||||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
47|Flóvenz et al., 2005|Kristinsdóttír et al., 2010|25.6.1995|Surface|Heiðmörk |364980|398695|-21.76651|64.06478|148||Ferskt nútíma hraun sem hefur alldrei komizt niður fyrir grunnvatnsborð. Staðsetning ónákvæm|"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|||8.33|Triple Weight|||||||1273|0.0007856|2.73E-03|0.048480005|100||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
58|Flóvenz et al., 2005|Kristinsdóttir et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarð|604229|577882|-16.73214|65.70167|606|187|Smáblöðrusóna.  Sjá borskýrslu Steingrímsson (1997)|See drilling report in Steingrímsson (1997)|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.70|Triple weight|||10.50|Scale and caliper|||||||485|0.0020628|1.07E-01|0.014588439|450||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
61|Flóvenz et al., 2005|Kristinsdóttir et al., 2010|13.6.1995|Borehole|Krafla KH-1, Sandabotnaskarð|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|||19.20|Triple Weight|||||||31|0.0319337|6.42E-01|0.014040764|85||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
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 farið niður fyrir grunnvatnsborð. Staðsetning ónákvæm. |"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|||11.70|Triple Weight|||||||1413|0.0007077|4.84E-03|0.01486217|72.6||Zahner IM-6 electrochemical workstation; measured over a range of frequencies||||||||
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 sýnið er af grunnu sjávar gosbreksíu eða móbergi í holu boraðri 2008 in vinnsluholu RN17-B af 2801,6 m dýpi. Hátt ummyndunarstig innan amfíból beltis. Móbergið er misleitt fínkorna tekstúr og grunnmassa og blörðotta mola. . Það er alummyndað með 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 Friðleifsson 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, sphène 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 Friðleifsson & Richter (2010).|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|3.00|Triple weight|||13.73|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.|5.25|4.94|3.11|2.54|0.3||22.1|17.7
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 fjallað er um í skýrslu Friðleifsson o.fl. 2010, voru kjarnar boraðir árið 2005 á 2238-2248 m dýpi. Sýni rannsakað við UM ir af 2246 m dýpi. Sýnið er úr dóleríti sem sýnir afar litla ummyndun. Og talið vera komið úr gangasveimi. Tekstúr er grófkorna og magmatískur. Sýnið er fremur ferskt og sýnir engar gasblörður. . dílarnir eru plagíóklas og klínó-pýroxen og er þar ásamt klóríti, talki, oxíði og kvartsi.  XRD og SEM/EBSD/EDS greiningar sýna tilveru þriggja steinda; plagíóklas, ágít og klórít aog smávegis af talki, aktínólíti og kvars. plagíóklas sýnir ummyndunarsprungurmeð anorthíti-andesíni. Klínópýroxeninn er af ágít samsetningu.  EBSD greining sýnir að ágítið og plagíóklas sýna óverulega kristalbyggingu eins og sýnt er á strerogrammi, sjá skýrslu IDDP-ICDP smákjarna  í Friðleifsson og RIchter 2010|As reported in Friðleifsson 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 Friðleifsson & Richter (2010).|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Chlorite-epidote|2.75|Triple weight|||1.25|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.|3.78|5.70|2.36|2.49|0.4||13.9|17.1
RN-30|Nono et al., 2020|Reinsch et al., 2016||Borehole|Reykjanes|318082|373572|-22.69545|63.86776|26|2519|Kjarnasýnið kemur úr holu RN-30 af 2519 m dýpi. Bergið er mikródólerít með plagíóklas, klínópýroxen, epidóti, kvars og oxíð ásamr ráðandi klórít ummyndun. Textúr er óreglulegur og gerður úr meðalkorna magmatísku bergi. Kristallar eru mjög óreglulega sprungnir eins og velsést í þunnsneiðum. magnummyndunarröðun (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 Friðleifsson 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 Friðleifsson & Richter (2010).|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|3.02|Triple weight|||2.90|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.|4.59|5.65|2.60|2.63|0.4||17.0|20.8
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 (50-100μm) pores are entirely filled with chlorite, whereas larger pores (up to 500μm) 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 μm) 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|||17.96|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.|4.31|4.28|2.51|2.11|0.3||12.8|11.4
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 neðan NJ-17) á Nesjavöllum Hengli háhitakerfinu. NJ-17B er ummyndað móberg, en er mjög klórít ríkt. Grunnmassinn er fínkorna aktínólít, klórít, plagíóklas og oxíð. Stórar ílangar porur eru fylltar af klóríti við jaðarinn og síðan kalsít, klínópýroxen og síðan oxíð og plagíóklas í miðjunni. óreglulegar oxíð æðar eru til staðar, ásamt klórít æðum. XRD griningar sýna fimm steindategundir. plagíóklas klórít, kalsít, aktínólít og ágít. Aktínólít hefur ekki fundist sem díll, og er líklegast að finna innan grunnmassans í tengslum við 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|||12.08|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.|4.52|4.56|2.67|2.29|0.3||15.7|14.2
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. Sýnið er ummyndað móbergstúff. Porur eru aðallega fylltar af klóríti. Ummyndunarútfellingar milli korna eru klórít, epidót, kvars, plagíóklas og kalsít, sum holými eru ekki fyllt. Rúnnuð korn sem eru nokkurra milimetra breið með dökku yfirborði. stór fínkorna molar hafa dökk oxíð, nanó-oxíð/súlfíð-nálar með óreglulegri stefnu.  sum kornin hafa óreglulegar sprungur (nokkurra hundraða microm og fáeina microm breiðar. sem fylltar eru kvarsi. stórir brúnir og grænir (sjaldséðara) fínkorna hópar af ""xenomorphic"" prisma nálum með nanó undirkonum úr epidóti og mögulega vaxið 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 μm long and few μm 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|||24.16|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.|3.88|3.97|2.31|2.09|0.3||10.3|10.6
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, tekið á 2804 m dýpi. Sýnið er mjög ummyndað í amfíból belti. Sýnið er algerlega ummyndað og með blöðrótt og þétt korn. Ríkt af fínkorna epidóti í plagíóklas og amfíól kristöllum. Porur sýna tengingu. Amfíból sést í fínkorna grunnmassa ásamt með meðalstórum blöðrum þar sem epidót og plagíóklas fylla. sumar blöðrur eru tómar í miðju þunnsneiðarinnar. XRD greiningar sýna þrjá 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|||13.56|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.|4.82|4.61|2.99|2.41|0.3||21.3|16.0
GG1-porDol|Reinsch et al., 2016||14.5.2014|Surface|Geitafell|673425|441169|-15.39855|64.42795|213||Breksíerað sýni tekið á mótum dílótts gabbró(dólerít) og umlykjandi basalts. Grænleitar 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|||1.22|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.||||||||
GG1-hrBa|Reinsch et al., 2016|||Surface|Geitafell|673541|441052|-15.39628|64.42685|194||Ummyndað basalt með kvarsi/kalsíti (epidóti?) í æðum.|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|||0.84|He gas pycnometry|||||||||||||||||||||
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|||4.21|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.||||||||
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|||7.89|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.||||||||
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|||1.23|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.||||||||
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|||2.78|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.||||||||
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|||0.87|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.||||||||
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|||0.56|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.||||||||
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|||0.55|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.||||||||
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|||27.85|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.||||||||
RN-17B|Reinsch et al., 2016|||Borehole|Reykjanes RN-17|318072|373574|-22.69566|63.86777|20||Misleit breksía með móbergs grunnmassa. |Heterolithic breccia with hyaloclastite matrix|Hyaloclastite|Hyaloclastite breccia|Epidote-actinolite|2.70|Triple weight|||13.64|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.||||||||
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|||3.24|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.||||||||
GrPhy-L|Reinsch et al., 2016|||Surface|Reykjanes|||||||Granófýr|Granophyre|Silicic intrusion|Granophyre|Unaltered|2.45|Triple weight|||8.30|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.||||||||
L02|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|40|Sambrædd breksía, Bergið er rauðleitara og aukning í fylltum sprungum. Mikið brotið og mjög ummyndað. Rík a zeólítum  og pýríti, mjög ummynduð. |Welded breccia; A lot of zeolites and pyrite, very altered|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.68|Triple weight|||35.99|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 μS/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|2.92|3.14|1.67|1.45||||
L05a|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|45|Mjög ummynduð morkin breksía. Dæmigerður HALARAUÐUR|Ignimbrite, very dense, low alteration level, iron rich|Silicic volcanic|Ignimbrite|Smectite-zeolite|2.71|Triple weight|||21.46|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 μS/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|4.24|4.30|2.59|2.20||||
L05b|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|45|Mjög ummynduð morkin breksía. Dæmigerður HALARAUÐUR|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|||6.54|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 μS/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|5.28|5.29|3.14|2.67||||
L06|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|49|Basaltbreksía með rauðum molum í og hvítsett af útfellingu, sem eru í blöðrum.|Basalt breccia with oxidized grains and whitish deposition in vesicles|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.62|Triple weight|||26.43|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 μS/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||||
L09|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|60|Basaltbreksía. Mjög morkið, mikið um pýrít. 20 gr. Sprunga. Mjög morkið og brotið.|Basalt breccia, very crumbly abundant pyrite, heavily fractured|Hyaloclastite|Hyaloclastite breccia|Smectite-zeolite|2.75|Triple weight|||27.45|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 μS/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|3.12|3.71|1.7|1.67||||
L10|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|66|Morkið fínk. Basalt|Crumbly fíne-grained basalt|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||30.15|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 μS/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|3.62|3.76|2.23|2.00||||
L11|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|69|Smáblöðrótt basalt. Straumflögótt, fínk. Basalt|FInely vesiculated basalt, flow lineated.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.90|Triple weight|||22.08|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 μS/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|4.04|4.08|2.46|1.96||||
L12a|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|70|Smáblöðrótt 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|||3.94|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 μS/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|5.36|5.67|3.23|2.92||||
L12b|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|70|Smáblöðrótt 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|||4.66|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 μS/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|5.47|5.76|3.17|2.93||||
L14|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|75|Morkið dökkgrátt túff|Hyaloclastite, crumbly and dark-grey|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.67|Triple weight|||39.48|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 μS/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|2.66|2.89|1.49|1.26||||
L15|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|80|Bergið grátt og morkið. Stakar stórar blöðrur.|Grey crumbly rock, occasional large vesicles. |Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.93|Triple weight|||10.50|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 μS/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|4.28|4.68|2.4|2.34||||
L16|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|99|Ljósgrænt, ummyndað og illa kristallað.|Light green altered and partially crystallized|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.83|Triple weight|||9.80|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 μS/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|4.34|4.77|2.66|2.35||||
L19|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|120|Fínkornað þétt basalt|Dense fíne grained lava|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||21.63|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 μS/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|4.01|4.19|2.32|2.04||||
L21|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|126|Dökk sónasprunga - utf. Oxað og þétt|Dark fracture, oxidized and dense|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||14.86|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 μS/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|4.11|4.51|2.18|2.18||||
L22|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|131|Blóðrótt illa kr. Basalt|Vesicular, poorly crystalline lava|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.80|Triple weight|||13.90|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 μS/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|4.19|4.40|2.23|2.16||||
L24a|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|144|Hólrými með plötukalsíti o. fl. Mobergið er þéttara 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|||22.16|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 μS/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|3.49|3.86|2.08|1.89||||
L24b|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|144|Hólrými með plötukalsíti o. fl. Mobergið er þéttara hér.|Same as L24a but drilled in a different direction to study anisotropy.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.80|Triple weight|||17.82|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 μS/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|4.12|2.19|1.92||||
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|||34.40|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 μS/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|3.17|3.33|2.2|1.60||||
L26|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|158|Bergið betur kristallað og er oxað.|Rock better crystalized and oxidized|Lava flow|Medium-coarse grained basaltic lava|Smectite-zeolite|2.89|Triple weight|||9.86|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 μS/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|5.14|5.44|2.64|2.63||||
L28|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|167|Fínk. grátt þétt basalt. Smá plag. dílar.|Fine grained dense basalt. Micro-plagioclase porphyritic|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.82|Triple weight|||13.57|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 μS/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|4.24|4.30|2.58|2.22||||
L29|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|174|Hraunlaga. Grátt. Oxað berg og blöðrur 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|||17.73|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 μS/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|4.52|4.94|2.66|2.42||||
L30|Levy et al., 2018|||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|185|Gangberg. Smáblöðrur raða sér í boga eins og um sprungu væri að ræða. |Dyke. Micro vesicles form a row |Basaltic intrusion|Fine-medium grained basaltic intrusion|Smectite-zeolite|2.85|Triple weight|||4.98|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 μS/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|5.19|5.15|2.74|2.70||||
L31|Levy et al., 2018|Levy et al., 2019a,b||Borehole|Krafla KH-1|604229|577882|-16.73214|65.70167|505|189|Útfellingaríkt grængrátt móbergstúff.|Extremely altered greyish green hyaloclastite tuff. |Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.77|Triple weight|||23.65|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 μS/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||||
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 gerð úr bergbrotum og með ljósum ummynðuðum glergrunnmassa, mikið pýrít og kalsít. Breksían er mishörð og með ""stringers"" eða þunnum þéttum basaltlögum. Orlítið finkornottari, annars sama bergið/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|||12.06|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 μS/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|4.53|4.67|2.73|2.18||||
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|||13.94|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 μS/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|4.73|5.15|2.85|3.08||||
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 blöðrótt og holufyllt, cc, qz, lau, heu. Æð eða 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|||24.79|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 μS/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|3.73|4.27|2.41|2.03||||
L40|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|190|Þétt kristallað ljósleitt berg líklega basalt andesít/andesít, flókin bortatextúr með nokkrar kynslóðir 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|||23.36|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 μS/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|4.02|3.85|2.33|2.11||||
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 víð a brotin, misgengisbort með slickenslides í 200,5 m, leir á brotfleti. Smásætt KVARTS og leir í blöðrum|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|||11.33|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 μS/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|5.37|5.56|2.98|2.99||||
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 blöðrótt berg. WAIRAKÍT finnst gyrst í 224 m dýpi og finnst síðan við a í blöðrum með kvartsi og eða plötulaga kalsíti. Bergið er frauðkennt í 226 m dýpi en þar kunna að 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|||30.61|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 μS/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|3.37|3.43|2.06|2.13||||
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 blöðrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöðrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöðrum 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|||18.27|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 μS/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|4.72|4.84|2.89|2.23||||
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 blöðrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöðrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöðrum 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|||21.37|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 μS/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|4.22|4.44|2.56|2.14||||
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 blöðrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöðrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöðrum 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|||27.09|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 μS/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|3.54|3.69|2.08|1.86||||
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 blöðrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöðrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöðrum 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|||24.36|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 μS/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|2.88|3.79|1.67|1.83||||
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 blöðrótt storkuberg líklega ísúr hraun (andesít). Wairakít í sprungum og blöðrum ásamt kvartsi. Leir á mörgum sprunguflötum. EPIDÓT finnst í blöðrum 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|||23.43|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 μS/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|3.01|3.87|1.52|1.77||||
L47|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|286|Dumbrauðleitt berg fínblöðrótt|Dark-red rock finely vesiculated|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.99|Triple weight|||23.97|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 μS/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|3.44|3.77|2.19|1.85||||
L48|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|288|Dumbrauðleitt berg fínblöðrótt|Dark-red rock finely vesiculated|Lava flow|Fine-medium grained basaltic lava|Chlorite-epidote|2.96|Triple weight|||20.55|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 μS/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|4.08|4.18|2.32|2.25||||
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 eða 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|||10.30|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 μS/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|4.52|5.02|2.85|3.46||||
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 eða 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|||23.18|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 μS/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|4.18|4.18|2.37|1.99||||
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 eða 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|||28.11|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 μS/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|3.83|3.92|2.41|1.97||||
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|||14.37|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 μS/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|4.75|4.67|2.79|2.32||||
L54|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|346|Þykk bólstrabergsmyndun, bólstrarnir eru með rauðleitri slikju og sitja í grænum velummynduðum grunnmassa. Þessia myndun er frekar einsleit hefst í um 327 m dýpi og nær niður 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|||15.92|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 μS/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|4.46|4.63|2.39|2.68||||
L55|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|357|Þykk bólstrabergsmyndun, bólstrarnir eru með rauðleitri slikju og sitja í grænum velummynduðum grunnmassa. Þessia myndun er frekar einsleit hefst í um 327 m dýpi og nær niður 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|||15.99|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 μS/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|3.86|4.50|2.33|2.35||||
L56|Levy et al., 2018|Gautason et al., 2007|3.12.2006|Borehole|Krafla KH-5|600972|578705|-16.80233|65.70345|471|366|Þykk bólstrabergsmyndun, bólstrarnir eru með rauðleitri slikju og sitja í grænum velummynduðum grunnmassa. Þessia myndun er frekar einsleit hefst í um 327 m dýpi og nær niður 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|||30.32|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 μS/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|3.68|3.74|2.21|1.89||||
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 (eða 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|||31.99|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 μS/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|3.72|3.59|2.13|1.84||||
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 þétt basaltinnskot. |Light fine-grained dense intrusion|Basaltic intrusion|Fine-medium grained basaltic intrusion|Chlorite-epidote|2.95|Triple weight|||12.65|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 μS/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|5.01|5.08|3.19|2.84||||
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 (eða 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|||21.95|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 μS/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|4.41|4.23|2.76|2.25||||
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 þunn innskot eða innskotsæðar í bólstrabreksíu.|A few thin basaltic intrusions or veins. Within a pillow breccia|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.85|Triple weight|||18.51|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 μS/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||||
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 þessari einingu en hlutfall bólstrabrota lækkar er neðar 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|||34.70|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 μS/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|2.85|3.09|1.64|1.49||||
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 með stórum ljósum bergrotum í miðhluta einingarinnar. |Hyaloclastite breccia with large basalt fragment within the central part of the unit. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.92|Triple weight|||18.52|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 μS/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|4.55|4.71|2.92|2.19||||
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 þétt efst en blöðróttara er neðar 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|||22.27|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 μS/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|4.42|4.44|2.55|2.33||||
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 með köntuðum 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|||25.23|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 μS/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|4.19|4.32|2.48|2.27||||
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 með köntuðum 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|||27.41|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 μS/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|3.99|4.27|2.36|2.27||||
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 með tltölulega ferskum basaltbrotum í garænum vel ummynduðum grunnmassa|Basalt breccia containing relatively fresh basalt fragments embedded in grayish-green altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.93|Triple weight|||34.65|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 μS/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|3.56|3.49|2.29|1.79||||
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 með tltölulega ferskum basaltbrotum í garænum vel ummynduðum grunnmassa|Basalt breccia containing relatively fresh basalt fragments embedded in grayish-green altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.91|Triple weight|||37.08|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 μS/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|3.69|3.50|2.28|1.94||||
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 smáblöðrótt berg, blöðrur liggja í taumum sem mynda 45 deg horn við borstefnu. Sprungur og sprugufyllingar eru nær samsíða blöðrutaumum|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|||30.97|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 μS/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|3.82|3.80|2.36|2.20||||
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 með tltölulega ferskum basaltbrotum í garænum vel ummynduðum grunnmassa|Hyaloclastite breccia with relatively fresh basalt fragments embedded in heavily altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.91|Triple weight|||24.71|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 μS/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|4.65|4.68|2.57|2.37||||
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 með tltölulega ferskum basaltbrotum í garænum vel ummynduðum grunnmassa|Hyaloclastite breccia with relatively fresh basalt fragments embedded in heavily altered groundmass. |Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.99|Triple weight|||9.89|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 μS/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|5.12|5.23|2.79|3.29||||
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 með óreglulegri blörudreifingu, hnígandi seig bráð, 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|||||15.97|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 μS/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||||||||||||4.43|5.10|2.64|2.81||||
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 blöðróttu holufylltu basalti, bergið dökknar er neðar dregur. Á köflum er kjarninn mikið sprungin og viða 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|||||10.66|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 μS/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|||||||||4.61|4.49|2.64|2.56||||
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 örþunnt innskot í 460 m - Síðan 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|||8.03|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 μS/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|5.06|5.14|2.74|2.63||||
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 með kvartsi og blaðlaga 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|||34.15|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 μS/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|4.27|4.11|2.52|2.60||||
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|Glerjað basalt. Hvítt WAIRAKÍT á eftir kvartsi í sprungufyllingu, einnig blaðlaga 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|||2.85|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 μS/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|3.72|3.60|2.09|1.82||||
L86|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|501|Glerjað basalt. Hvítt WAIRAKÍT á eftir kvartsi í sprungufyllingu, einnig blaðlaga kalsít|Glassy basalt, wairakite following quartz in a vein filling, also platy calcite.|Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|||||7.60|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 μS/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|||||||||3.33|3.49|1.87|1.55||||
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|||23.68|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 μS/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|4.03|4.72|2.67|2.35||||
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|||||11.31|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 μS/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||||
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|||11.09|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 μS/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|4.87|5.09||||||
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|||23.99|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 μS/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|3.35|1.64|3.11|1.45||||
L95|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|560|Breksía með litlum oft rúnnuðum bólstrabrotum í grænum 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|||||24.36|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 μS/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||||
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 með litlum oft rúnnuðum bólstrabrotum í grænum 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|||27.92|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 μS/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|3.31|1.77|3.31|1.54||||
L97|Escobedo, 2018|Gautason et al., 2007|1.2.2006|Borehole|Krafla KH-6|600969|580818|-16.80080|65.72240|513|582|Breksía með litlum oft rúnnuðum bólstrabrotum í grænum 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|||||25.14|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 μS/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|||||||||2.37|1.50|3.37|1.60||||
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 með litlum oft rúnnuðum bólstrabrotum í grænum 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|||30.54|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 μS/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|4.27|2.57|4.37|2.35||||
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 með litlum oft rúnnuðum bólstrabrotum í grænum 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|||24.76|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 μS/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|3.98|2.07|4.37|2.35||||
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 með rúnnuðum litlum bólstrabrotum, sem eru ljósgrá og frekar ferskleg, í grænum ummynduðum 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|||25.34|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 μS/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|3.16|1.90|3.94|1.98||||
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. Þykk bólstrabergsmyndun, örlítið af grænum 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|||16.99|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 μS/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|4.29|2.48|4.32|2.22||||
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|Þunnar innskotsæðar (eða hugsanlega stór bólstri) í 724,5 m (40 cm þykk) og í 735 m (30 cm þykk) bergíð er þétt 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|||12.43|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 μS/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|4.27|2.51|4.36|2.21||||
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 niður í botn holunnar. Bólstrabrot eru frekar ferskeleg en millimassin er grænn og vel ummyndaður. Í blöðrum 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|||21.08|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 μS/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|4.39|2.10|4.5|2.34||||
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|Þunnu hraunlagi|Thin basaltic lava |Lava flow|Fine-medium grained basaltic lava|Unaltered|3.00|Triple weight|||1.87|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 μS/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|6.41|6.47||||||
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 þunnu hraunlagi með 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|||36.63|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 μS/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|3.34|2.98||||||
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 nær blöðrulaust en mikið sprungið|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|||5.92|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 μS/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|5.49|5.86||||||
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|||4.30|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 μS/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|5.61|5.97||||||
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|||15.36|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 μS/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|3.67|3.86||||||
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|||5.09|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 μS/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||||||
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|Smáblöðrótt basalt|Doleritic dyke moderately altered and argilized|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.85|Triple weight|||4.18|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 μS/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|5.13|5.55||||||
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|Smáblöðrótt basalt|Doleritic dyke very altered and argilized|Basaltic intrusion|Medium-coarse grained basaltic intrusion|Mixed-layer clay|2.92|Triple weight|||9.85|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 μS/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|4.87|5.29||||||
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 frauðkenndara 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|||7.34|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 μS/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|4.91|5.39||||||
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 með óreglulegri blöðrudreifingu, hnígandi seig bráð, 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|||14.82|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 μS/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|4.31|4.67||||||
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|þétt 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|||11.27|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 μS/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|4.91|5.19||||||
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|þétt 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|||5.11|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 μS/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|5.72|5.98||||||
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|þétt 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|||4.89|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 μS/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|5.78|6.01||||||
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 grænleitur og talsvert mikið af leir. Allar holur og holrými eru með 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|||26.90|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 μS/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|2.58|3.29||||||
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. Þessi 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|||39.04|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 μS/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|3.06|2.91||||||
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. Þessi 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|||40.13|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 μS/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|2.79|2.73||||||
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 túffið, vægar ásýndarbreytingar, kornastærð sveiflast til, og við eru linsur með grófara efni, en allt sama túffið.|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|||38.69|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 μS/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|2.94|2.75||||||
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|Gríðarlega mikið pýrít. Neðar verður breyting og þar tekur við fínkorna móbergstúff, mikill leir, mikið pýrít.|A lot of pyrite, lot of clay. Fine grained hyaloclastite.|Hyaloclastite|Hyaloclastite tuff|Smectite-zeolite|2.74|Triple weight|||36.54|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 μS/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||||||
L200|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|142.4|"Flott breksía, mest gerð úr bergbrotum og með ljósum ummynðuðum glergrunnmassa, mikið pýrít og kalsít. Breksían er mishörð og með ""stringers"" eða þunnum þéttum basaltlögum. Orlítið finkornottari, annars sama bergið/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|||30.95|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 μS/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|3.51|2.27|3.62|1.80||||
L201|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|153.5|Bólstrabrot eða stór steinn. |Pillow piece or large fragment. |Lava flow|Fine-medium grained basaltic lava|Mixed-layer clay|2.70|Triple weight|||6.60|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 μS/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|4.64|2.78|4.64|2.44||||
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 komið í fínkorna túff, fín-lagskipt hálfgert set-túff og ummyndun minnkar. Túffið 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|||22.56|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 μS/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|5.27|2.99|5.42|2.65||||
L203|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|160.8|Basalttúff með bergbrotum|Basaltic tuff with rock fragments. |Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.68|Triple weight|||33.96|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 μS/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|3.26|1.74|5.2|2.16||||
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|||25.17|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 μS/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||||
L205|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|185.2|Steinar eða stringers, í túffinu -- sem er að það sama of að ofan.|Minerals or stringers in tuff, same as above.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.73|Triple weight|||24.57|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 μS/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|1.63|1.03|2.08|1.21||||
L206|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|192.4|Græn leirdrulla, líklega millilag, eða kargi.|Interlayer or flow-top breccia, green clay.|Lava flow|Flow-top breccia|Mixed-layer clay|2.75|Triple weight|||17.54|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 μS/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|5.56|3.15|5.72|2.86||||
L207|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|204.2|Fín-meðalkorna basalt.|Fine-medium grained basalt|Lava flow|Fine-medium grained basaltic lava|Unaltered|2.93|Triple weight|||22.43|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 μS/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|2.35|1.24|2.31|1.59||||
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|||25.76|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 μS/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|2.66|1.55|2.68|1.64||||
L209|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|234.7|Túff breksía, mikið af basalti|Tuff breccia, lot of basalt|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.55|Triple weight|||19.25|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 μS/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|2.61|1.49|2.62|1.51||||
L210|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|246.5|Mjög fínkorna túff, með miklum perlitiskum textúr. Gjóskutúff, svolítið 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|||22.05|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 μS/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|2.94|1.75|3|1.66||||
L211|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|262.7|Móbergtúff, fínkorna með talsvert miklu af bergbrotum.|Hyaloclastite tuff, fine grained with a lot of broken pieceS.|Hyaloclastite|Hyaloclastite tuff|Mixed-layer clay|2.57|Triple weight|||17.60|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 μS/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|3.75|2.25|3.47|2.27||||
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, pyþ|Breccia. No clear layering, rather gradient. Laumontite, analcime, calcite, pyrite.|Hyaloclastite|Hyaloclastite breccia|Mixed-layer clay|2.84|Triple weight|||19.85|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 μS/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|4.53|2.67|4.57|2.34||||
L213|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|318.7|Ljóst þétt, sprungið og vöðlað, gæti verið rhyólít, eða ummyndað brotaberg.|Light, compact, fractured. Could be rhyolite or altered broken rock|Silicic volcanic|Rhyolite breccia|Chlorite-epidote|2.69|Triple weight|||25.99|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 μS/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|4.91|2.65|5.41|2.46||||
L214|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|362.5|Breksía mikið laumontít.|Breccia with lot of laumontite|Hyaloclastite|Hyaloclastite breccia|Chlorite-epidote|2.71|Triple weight|||14.67|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 μS/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|4.87|2.66|5.57|2.71||||
L215|This study|Jónsson et al., 2003||Borehole|Krafla KH-3|606657|580693|-16.67711|65.72609|590|377.8|Einsleitt basalt, bokkuð blöðrótt beltar blöðrusónur, líklega hraunlagasyrpa.|Homogenous basalt, little alteration.|Lava flow|Fine-medium grained basaltic lava|Smectite-zeolite|2.86|Triple weight|||5.54|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 μS/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|2.85|1.34|3.29|1.37||||
L216|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||5.24|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 μS/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||||
L217|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||14.03|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 μS/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|4.71|2.76|4.79|2.91||||
L218|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||46.81|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 μS/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|5.39|3.05|5.53|3.17||||
L219|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||2.78|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 μS/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|5.56|3.15|5.72|2.86||||
L222|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||48.24|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 μS/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|2.35|1.24|2.31|1.59||||
L223|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||46.89|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 μS/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|2.66|1.55|2.68|1.64||||
L225|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||39.55|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 μS/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|2.61|1.49|2.62|1.51||||
L226|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||35.00|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 μS/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|2.94|1.75|3|1.66||||
L227|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||30.28|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 μS/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|3.75|2.25|3.47|2.27||||
L228|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||15.69|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 μS/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|4.53|2.67|4.57|2.34||||
L229|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||7.71|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 μS/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|4.91|2.65|5.41|2.46||||
L230|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||4.73|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 μS/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|4.87|2.66|5.57|2.71||||
L231|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||25.82|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 μS/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|2.85|1.34|3.29|1.37||||
L232|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||16.46|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 μS/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||||
L233|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||14.54|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 μS/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|4.71|2.76|4.79|2.91||||
L234|This study|Lacasse et al. (2007)|4.7.2011|Borehole|Theistareykir ÞR-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|||3.04|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 μS/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|5.39|3.05|5.53|3.17||||
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|||2.90|Triple weight|||||||2421|0.0004130|0.00039|0.063|322|||4.654|5.949|2.734|3.197||||
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|||2.70|Triple weight|||||||1524|0.0006561|0.00074|0.063|330|||5.111|6.156|3.203|3.337||||
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|||2.70|Triple weight|||||||1832|0.0005457|0.00035|0.063|235|||5.068|6.286|3.066|3.425||||
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|||2.20|Triple weight|||||||1321|0.0007568|0.00049|0.063|207|||4.758|5.961|2.778|3.419||||
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|||1.80|Triple weight|||||||1327|0.0007536|0.00038|0.063|218|||4.372|6.036|2.747|3.035||||
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|||1.70|Triple weight|||||||1077|0.0009289|0.00055|0.063|159|||4.272|5.754|2.489|2.96||||
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|||1.80|Triple weight|||||||1447|0.0006911|0.00043|0.063|195|||3.982|5.856|2.506|3.104||||
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|||2.00|Triple weight|||||||1360|0.0007350|0.00056|0.063|188|||4.095|5.684|2.519|2.939||||
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|||2.00|Triple weight|||||||1103|0.0009064|0.00085|0.063|201|||4.196|5.78|2.58|2.955||||
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|||2.00|Triple weight|||||||1798|0.0005560|0.00038|0.063|223|||4.422|5.743|2.622|2.965||||
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|||2.20|Triple weight|||||||1325|0.0007547|0.00058|0.063|184|||4.553|5.804|2.759|3.229||||
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|||1.80|Triple weight|||||||846|0.0011819|0.00078|0.063|182||||5.245||2.577||||
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|||0.30|Triple weight|||||||8479|0.0001179|0.00015|0.063|640|||5.921|6.69|3.541|3.592||||
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|||0.90|Triple weight|||||||2167|0.0004614|0.00044|0.063|270|||4.569|5.965|2.841|3.102||||
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|||2.70|Triple weight|||||||||||-|||2.36|4.617|1.486|2.146||||
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|||2.50|Triple weight|||||||817|0.0012241|0.00015|0.063|64|||2.546||1.509|||||
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|||2.80|Triple weight|||||||872|0.0011467|0.00062|0.063|94|||2.339|4.69|1.51|||||
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|||2.90|Triple weight|||||||905|0.0011053|0.0003|0.063|92|||2.315|4.944|1.319|2.566||||
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|||1.70|Triple weight|||||||1319|0.0007583|0.00031|0.063|123|||4.24|5.505|2.569|3.046||||
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|||1.50|Triple weight|||||||1139|0.0008780|0.00052|0.063|162|||4.303|5.539|2.611|2.888||||
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|||1.50|Triple weight|||||||1474|0.0006783|0.00044|0.063|161|||4.646|5.652|2.838|||||
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|||1.6000|Triple weight|||||||893|0.0011200|0.001|0.09|200|||5.227|6.35|2.951|2.95|0.3||64.6|25.0
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|||1.6000|Triple weight|||||||709|0.0014100|0.0019|0.09|111|||4.36|6.18|2.439|2.75|0.3||43.5|17.1
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|||1.8000|Triple weight|||||||1144|0.0008740|0.0009|0.09|111|||5.464|6.40|2.735|2.83|0.3||55.8|21.3
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