<?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>Stan E. Church</dc:contributor>
  <dc:contributor>Philip L. Verplanck</dc:contributor>
  <dc:contributor>Laurie Wirt</dc:contributor>
  <dc:creator>Douglas B. Yager</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>During 1996 to 2000, the Bureau of Land Management, National &#13;
      Park Service, Environmental Protection Agency, United States &#13;
      Department of Agriculture (USDA) Forest Service, and the &#13;
      U.S. Geological Survey (USGS) developed a coordinated &#13;
      strategy to (1) study the environmental effects of &#13;
      historical mining on Federal lands, and (2) remediate &#13;
      contaminated sites that have the greatest impact on water &#13;
      quality and ecosystem health.  This dataset provides &#13;
      information that contributes to these overall objectives and &#13;
      is part of the USGS Abandoned Mine Lands Initiative.  Data &#13;
      presented here represent ferricrete occurrences and selected &#13;
      iron bogs and springs in the upper Animas River watershed in &#13;
      San Juan County near Silverton, Colorado.  Ferricretes &#13;
      (stratified iron and manganese oxyhydroxide-cemented &#13;
      sedimentary deposits) are one indicator of the geochemical &#13;
      baseline conditions as well as the effect that weathering of &#13;
      mineralized rocks had on water quality in the Animas River &#13;
      watershed prior to mining.  Logs and wood fragments &#13;
      preserved in several ferricretes in the upper Animas River &#13;
      watershed, collected primarily along streams, yield &#13;
      radiocarbon ages of modern to 9,580 years B.P. (P.L. &#13;
      Verplanck, D.B. Yager, and S.E. Church, work in progress).  &#13;
      The presence of ferricrete deposits along the current stream &#13;
      courses indicates that climate and physiography of the &#13;
      Animas River watershed have been relatively constant &#13;
      throughout the Holocene and that weathering processes have &#13;
      been ongoing for thousands of years prior to historical &#13;
      mining activities.  Thus, by knowing where ferricrete is &#13;
      preserved in the watershed today, land-management agencies &#13;
      have an indication of (1) where metal precipitation from &#13;
      weathering of altered rocks has occurred in the past, and &#13;
      (2) where this process is ongoing and may confound &#13;
      remediation efforts.&#13;
      These data are included as two coverages-a ferricrete &#13;
      coverage and a bogs and springs coverage.  The coverages are &#13;
      included in ArcInfo shapefile and ArcInfo interchange file &#13;
      format.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/mf2406</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Ferricrete, manganocrete, and bog iron occurrences with selected sedge bogs and active iron bogs and springs in the upper Animas River watershed, San Juan County, Colorado</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>