<?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>J.V. Gardner</dc:contributor>
  <dc:contributor>A. E. Jennings</dc:contributor>
  <dc:contributor>B. D. Edwards</dc:contributor>
  <dc:creator>M.E. Field</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>On Nov. 8, 1980, a major earthquake (magnitude 6.5-7.2) occurred 60 km off the coast of N California. A survey of the area using high-resolution seismic-reflection and side-scan sonar equipment revealed the presence of extensive sediment failure and flows in a zone about 1 km wide and 20 km long that trends parallel to the shelf on the very gently sloping (less than 0.25o) Klamath River delta.-from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>Earthquake-induced sediment failures on a 0.25o slope, Klamath River delta, California.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>