<?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>A.M. Sarna-Wojcicki</dc:contributor>
  <dc:contributor>R.S. Thompson</dc:contributor>
  <dc:creator>D.B. Madsen</dc:creator>
  <dc:date>2002</dc:date>
  <dc:description>A newly identified tephra in stratified deposits in southwestern Utah, dated ???14,000 14C yr B.P., may aid in correlating late Pleistocene deposits across parts of the southern Great Basin and west-central Colorado Plateau. Geochemical analyses of the ash suggest the tephra originated from Mono Craters, California, and most probably correlates with Wilson Creek ash #3. Because the ash is 2 mm thick ???550 km from its source, the event may have been larger than others correlated to Mono Craters eruptions. ?? 2002 University of Washington.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1006/qres.2002.2326</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>A late Pleistocene tephra layer in the southern Great Basin and Colorado Plateau derived from Mono Craters, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>