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Vulcanology: Interaction between Kilauea and Mauna Loa

Miklius, Asta; Cervelli, Peter


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  <dc:creator>Miklius, Asta</dc:creator>
  <dc:creator>Cervelli, Peter</dc:creator>
  <dc:date>2003-01-16</dc:date>
  <dc:description>After almost a decade of very slow rates of deformation, Mauna Loa in Hawaii, the largest volcano on Earth, began inflating in May 2002; at the same time, a high-volume effusive episode began at its neighbour Kilauea. We have found a correlation between these events at a very short timescale, detected by continuous deformation monitoring. This remarkable observation suggests that there is a crustal-level interaction between the magma systems of Mauna Loa and Kilauea, reviving a century-old controversy over the relationship between these two volcanoes on the basis of differences in their lava chemistry and in their patterns of eruptive behaviour1,2,3,4,5.</dc:description>
  <dc:identifier>https://zenodo.org/record/1233225</dc:identifier>
  <dc:identifier>10.1038/421229a</dc:identifier>
  <dc:identifier>oai:zenodo.org:1233225</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>https://creativecommons.org/publicdomain/zero/1.0/legalcode</dc:rights>
  <dc:title>Vulcanology: Interaction between Kilauea and Mauna Loa</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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