<?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>E.B. Nuhfer</dc:contributor>
  <dc:contributor>W.E. Dean</dc:contributor>
  <dc:creator>R.Y. Anderson</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Volcanic ash from the eruption of Mount St. Helens on 18 May 1980 fell into Williams Lake in eastern Washington and was temporarily suspended at the sediment-water interface. After several months of compaction, the ash layer broke up and sank into lower density uncompacted lake sediment. Stratigraphic time displacements of several hundred years and a failure to recognize discontinuous ash layers in sediment cores are possible consequences of this process.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.225.4661.505</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Sinking of volcanic ash in uncompacted sediment in Williams Lake, Washington</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>