<?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>David S. Fullerton</dc:contributor>
  <dc:contributor>David L. Weide</dc:contributor>
  <dc:creator>Gerald M. Richmond</dc:creator>
  <dc:date>1987</dc:date>
  <dc:description>The Quaternary Geologic Map of the Chesapeake Bay 4? x 6? Quadrangle&#13;
      was mapped as part of the Quaternary Geologic Atlas of the United States.&#13;
      The atlas was begun as an effort to depict the areal distribution of&#13;
      surficial geologic deposits and other materials that accumulated or&#13;
      formed during the past 2+ million years, the period that includes all&#13;
      activities of the human species.  These materials are at the surface of&#13;
      the Earth.  They make up the 'ground' on which we walk, the 'dirt' in&#13;
      which we dig foundations, and the 'soil' in which we grow crops.  Most&#13;
      of our human activity is related in one way or another to these surface&#13;
      materials that are referred to collectively by many geologists as&#13;
      regolith, the mantle of fragmental and generally unconsolidated material&#13;
      that overlies the bedrock foundation of the continent.  The maps were&#13;
      compiled at 1:1,000,000 scale.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i1420(NJ18)</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Quaternary geologic map of the Chesapeake Bay 4 degrees x 6 degrees quadrangle, United States</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>