<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>R. B. Moore</dc:contributor>
  <dc:contributor>Anon</dc:contributor>
  <dc:creator>Jim Kauhikaua</dc:creator>
  <dc:date>1993</dc:date>
  <dc:description>Exploitation of hydrothermal systems on active basaltic volcanoes poses some unique questions about the role of volcanism and hydrothermal system evolution. Volcanic activity creates and maintains hydrothermal systems while earthquakes create permeable fractures that, at least temporarily, enhance circulation. Magma and water, possibly hydrothermal water, can interact violently to produce explosive eruptions. Finally, we speculate on whether volcanic behavior can be affected by high rates of heat extraction.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Publ by Geothermal Resources Council</dc:publisher>
  <dc:title>Dynamic behavior of Kilauea Volcano and its relation to hydrothermal systems and geothermal energy</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>