<?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. M. Batson</dc:contributor>
  <dc:contributor>H. E. Holt</dc:contributor>
  <dc:contributor>E. C. Morris</dc:contributor>
  <dc:contributor>J. J. Rennilson</dc:contributor>
  <dc:contributor>E. A. Whitaker</dc:contributor>
  <dc:creator>E.M. Shoemaker</dc:creator>
  <dc:date>1967</dc:date>
  <dc:description>Surveyor V landed in a small crater, 8.5 meters wide and 12.5 meters long, which was probably formed by drainage of surficial fragmental debris into a subsurface fissure. The lunar surface debris layer is exposed in the walls of this crater. At depths below about 10 centimeters, the debris appears to be composed mainly of shock-compressed aggregates, ranging from a few millimeters up to 3 centimeters in diameter, set in a matrix of less-coherent finer particles. Rocky chips and fragments larger than a millimeter are dispersed as a subordinate constituent of the debris.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.158.3801.642</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Surveyor V: Television pictures</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>