<?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>James M. Robb</dc:contributor>
  <dc:contributor>John C. Behrendt</dc:contributor>
  <dc:creator>John Schlee</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;A bathymetric map based on new data allows examination&amp;nbsp;of geomorphic features on the narrow continental margin off Liberia.&amp;nbsp;The continental shelf in this region is relatively flat and featureless. The&amp;nbsp;northwestern part of the continental slope, off Monrovia and Cape&amp;nbsp;Mount, shows complex slump features and two submarine valleys. The&amp;nbsp;central part of the slope is smoother, apparently as a result of&amp;nbsp;progradation. The southeastern part of the slope, near Cape Palmas, is&amp;nbsp;crossed oblique to the shoreline by a structural valley that has been&amp;nbsp;modified by large slumps or landslides. This valley may be the&amp;nbsp;termination, at the continental margin, of an oceanic fracture zone. The&amp;nbsp;major slumplike features of the Liberian continental margin appear to&amp;nbsp;be surface manifestations of deep faulting which has been partially&amp;nbsp;masked by sedimentation.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Bathymetry of the continental margin off Liberia, West Africa</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>