<?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>R.H. Bennett</dc:contributor>
  <dc:contributor>B.A. Mc Gregor</dc:contributor>
  <dc:contributor>L.E. Shephard</dc:contributor>
  <dc:creator>G. Almagor</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>Stability analysis, based on infinite slope analysis and geotechnical data from a suite of 34 cores collected from the continental slope between Wilmington and Lindenkohl Canyons, indicates that the Quaternary surficial silty clay sediments on gentle slopes are stable; that sediment stability on steeper slopes (14??-19??) is marginal; and that on precipitous slopes (&gt;50??) only a thin veneer of unconsolidated sediments can exist. Small earthquake-induced accelerations or the effects of internal waves can result in slope sediment instabilities. ?? 1982 A. M. Dowden, Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02462753</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>