<?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>Thomas P. Miller</dc:contributor>
  <dc:contributor>Richard P. Emanuel</dc:contributor>
  <dc:contributor>Frederic H. Wilson</dc:contributor>
  <dc:creator>M. Elizabeth Yount</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>&lt;p&gt;The more prominent of the two visible intracaldera cones of Mount Veniaminof went into eruption in early June 1983 and continued until early April 1984. Veniaminof is a 2,507-m-high composite cone having an 8 x 11-km summit caldera which formed 3,300-3,700 yr B.P. (Miller and Smith, 1977). The active 1.6x1.2-km cone protrudes 200 m through the glacial ice filling the caldera; it lies in a 60-m-long belt of cinder cones that is transverse to the trend of the Aleutian arc (fig. 44). &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/70180231</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in &lt;i&gt;The United States Geological Survey in Alaska: Accomplishments during 1983&lt;/i&gt;</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>