<?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>Robert I. Tilling</dc:contributor>
  <dc:contributor>Robin T. Holcomb</dc:contributor>
  <dc:contributor>Fred W. Klein</dc:contributor>
  <dc:contributor>Arnold T. Okamura</dc:contributor>
  <dc:contributor>Donald W. Peterson</dc:contributor>
  <dc:creator>John P. Lockwood</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>The purpose of this paper is to present a complete account of contrasting yet related eruptions, thus filling a gap in the published narratives of recent activity of Kilauea; and to examine their significance within a broader context of regional magmatic and eruptive dynamics. We have gained a historical perspective and can view these three eruptions within a multidecade context of the eruptive behavior of not only Kilauea, but also of the adjacent Mauna Loa.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/pp1613</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Dept. of the Interior, U.S. Geological Survey ;Information Services [distributor],</dc:publisher>
  <dc:title>Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>