<?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>D. K. Harrison</dc:contributor>
  <dc:creator>R. A. Ayuso</dc:creator>
  <dc:date>1983</dc:date>
  <dc:description>&lt;p&gt;The Lye Brook Wilderness contains no significant mineral deposits. Although the Cheshire Quartzite is a&amp;nbsp;potential source of low-grade silica sand and crops out in a large area within the wilderness, its degree of&amp;nbsp;induration and relative inaccessibility make its use prohibitive. No major concentation of base metals exist within&amp;nbsp;the Precambrian rocks, although they contain the highest metal concentrations within the wilderness. Uranium&amp;nbsp;mineralization is not extensive in the Precambrian rocks, despite the occurrence of significant deposits nearby.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/mf1609C</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Mineral resource potential map of the Lye Brook Wilderness, Bennington and Windham counties, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>