<?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:creator>Samuel Woods Stewart</dc:creator>
  <dc:date>1956</dc:date>
  <dc:description>Ogden Valley is a northwest trending valley within the Wasatch Mountains &#13;
of north-central Utah. On the basis of geological evidence Ogden Valley is &#13;
believed to be structurally controlled by normal faults along both the east &#13;
and west margins. Gravity measurements in the valley definitely indicate a &#13;
fault with at least 2000 feet of vertical displacement along the west margin &#13;
of the valley. A fault with at least 1000 feet of vertical displacement is &#13;
postulated along the east margin of the valley, together with three smaller, &#13;
buried faults within the valley. The maximum depth of Quaternary alluvium &#13;
and Tertiary sediments within the valley is about 6000 feet.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr56112</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey],</dc:publisher>
  <dc:title>Gravity survey of Ogden Valley, Weber County, Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>