<?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>Steven M. Condon</dc:contributor>
  <dc:contributor>Karen J. Franczyk</dc:contributor>
  <dc:contributor>S. Don Brown</dc:contributor>
  <dc:creator>Alfred L. Bush</dc:creator>
  <dc:date>1983</dc:date>
  <dc:description>&lt;p&gt;The mineral resource potential of the Piedra Wilderness Study Area is low. No occurrences of metallic&amp;nbsp;minerals, of valuable industrial rocks and minerals, or of useful concentrations of organic fuels are known in the&amp;nbsp;study area. However, a noneconomic occurrence of gypsum in the Jurassic Wanakah Formation lies a few hundred&amp;nbsp;feet west of the WSA boundary, is believed to extend into the WSA, and has a low resource potential. Particular&amp;nbsp;attention was paid to the possible occurrence of organic fuels in the Pennsylvanian Hermosa Formation, of&amp;nbsp;uranium and vanadium in the Jurassic Entrada Sandstone and Morrison Formation, and of coal in the Cretaceous&amp;nbsp;Dakota Sandstone. Thin coaly beds in the Dakota have a low resource potential. Extensive sampling of stream&amp;nbsp;sediments, limited sampling of rock outcrops and springs, and a number of scintillometer traverses failed to&amp;nbsp;pinpoint significant anomalies that might be clues to mineral deposits.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/mf1630A</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Mineral resource potential of the Piedra Wilderness Study Area, Archuleta and Hinsdale counties, Colorado</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>