<?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. M. Myrick</dc:contributor>
  <dc:contributor>W. W. Emmett</dc:contributor>
  <dc:creator>R.H. Meade</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>Bed elevations were measured every 1 to 5 days during 10 consecutive weeks which included the peak snowmelt runoff, at 43 cross sections in a 1.83-kilometer reach of the East Fork River, Wyoming. Considerable scour and fill were recorded at many of the cross sections. (USGS)</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr82360</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey,</dc:publisher>
  <dc:title>Field data describing the movement and storage of sediment in the East Fork River, Wyoming; Part IV, bed elevation, 1980</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>