<?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>N. R. Gadd (compiler)</dc:contributor>
  <dc:contributor>J.J. Veillette</dc:contributor>
  <dc:contributor>P.W. Wagner</dc:contributor>
  <dc:contributor>W.F. Chapman</dc:contributor>
  <dc:creator>David S. Fullerton</dc:creator>
  <dc:date>1993</dc:date>
  <dc:description>The Quaternary Geologic Map of the Ottawa 4 degree x 6 degree Quadrangle&#13;
      was mapped as part of the Quaternary Geologic Atlas of the United&#13;
      States. The atlas was begun as an effort to depict the areal&#13;
      distribution of surficial geologic deposits and other materials that&#13;
      accumulated or formed during the past 2+ million years, the period that&#13;
      includes all activities of the human species.  These materials are at&#13;
      the surface of the earth.  They make up the 'ground' on which we walk,&#13;
      the 'dirt' in which we dig foundations, and the 'soil' in which we grow&#13;
      crops.  Most of our human activity is related in one way or another to&#13;
      these surface materials that are referred to collectively by many&#13;
      geologists as regolith, the mantle of fragmental and generally&#13;
      unconsolidated material that overlies the bedrock foundation of the&#13;
      continent.  The maps were compiled at 1:1,000,000 scale.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i1420(NL18)</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Quaternary geologic map of the Ottawa 4 degrees x 6 degrees quadrangle, United States and Canada</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>