<?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>L. C. Rowan</dc:creator>
  <dc:date>1971</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="TextRun SCXW125339220 BCX8" lang="EN-US" xml:lang="EN-US" data-contrast="auto"&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;The map shows the regional &lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;geology of the &lt;/span&gt;&lt;span class="SpellingError SCXW125339220 BCX8"&gt;Oppolzer&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; A region of the moon, where potential Apollo landing site&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;s 3 and 3R are located. Site 3R includes a prominent mare ridge and is of greater scientific interest (Trask, 1969). The &lt;/span&gt;&lt;span class="SpellingError SCXW125339220 BCX8"&gt;Oppolzer&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; A region is in Sinus &lt;/span&gt;&lt;span class="SpellingError SCXW125339220 BCX8"&gt;Medii&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;, near the center of the lunar earthside hemisphere; it is als&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;o&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; important because surve&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;yor VI successfully landed near the proposed Apollo landing areas.&lt;/span&gt; &lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;Sinus &lt;/span&gt;&lt;span class="SpellingError SCXW125339220 BCX8"&gt;Med&lt;/span&gt;&lt;span class="SpellingError SCXW125339220 BCX8"&gt;ii&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; is a relatively small, densely cratered &lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;mare&lt;/span&gt; &lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;surrounded by terra plains and sculptured terra&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; (&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;Wilhelms&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;, 1968). The geology of the region is dominated by a rela&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;tively high density of individual &lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt;craters and crater clusters. Most of the craters&lt;/span&gt;&lt;span class="NormalTextRun SCXW125339220 BCX8"&gt; are less than 800 meters in diameter and appear to be of secondary and primary impact origin.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i620</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Geologic map of the Oppolzer A region of the Moon Lunar Orbiter Site II P-8, Sinus Medii including Apollo landing sites 3 and 3R</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>