<?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>K. A. Howard</dc:contributor>
  <dc:contributor>H. G. Wilshire</dc:contributor>
  <dc:creator>D.E. Wilhelms</dc:creator>
  <dc:date>1979</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="TextRun SCXW63636780 BCX8" lang="EN-US" xml:lang="EN-US" data-contrast="auto"&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;The &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;map of the lunar region below &lt;/span&gt;&lt;span class="SpellingError SCXW63636780 BCX8"&gt;lat&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; 45&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;˚&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; S. is the &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;sixth part of a complete geolog&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;ic recon&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;naissance mapping of the moon at 1:5,000,000 scale. &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;The upper half of the map portrays the geology of the earth-facing or near side, and the lower half shows terrain that was unknown&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; before spacecr&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;aft photography. The near side that was well photographed&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; at &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;resolutions&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; of 0.1 to 0.5 km by Lunar Orbiter IV, but &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;coverage&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; of the far side is uneven quality&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; (fig. 1). The geology of a small area near the south pole that was in shadow during the &lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt;Orbiter&lt;/span&gt;&lt;span class="NormalTextRun SCXW63636780 BCX8"&gt; missions can be partly inferred from the nature of adjacent units.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i1162</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Geologic map of the south side of the Moon</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>