<?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:creator>A. P. Schultz</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;The zone of rockslides, identified by anomalous topography and geologic structures, is about 25 km long and 1.0 km wide. Downslope transport, ranging from 0.5 to 1.0 km, of at least 100 million m3 of Silurian sandstones and shales can be identified.-from Author&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0091-7613(1986)14&lt;11:AGRSCM&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Ancient giant rockslides, Sinking Creek Mountain, southern Appalachians, Virginia.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>