<?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>S.E. Dwornik</dc:contributor>
  <dc:creator>E. C. Morris</dc:creator>
  <dc:date>1978</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="TextRun SCXW24164227 BCX8" lang="EN-US" xml:lang="EN-US" data-contrast="auto"&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;The &lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;Amazonis&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt; quadrangle lies within the northern sparsely cratered hemisphere of Mars (&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;Carr&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt; and others, 19&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;73) The dominant structural ad physiographic features of the quadrangle are low feature&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;-&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;less plains (&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;Amazonis&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt; Planitia) in the center &lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;third of the quadrangle, the western flanks of the large volcanic construct, Olympus Mons, and its associated aureole deposits (Lycus Sulci&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;), which lies on the eastern slopes of the plains, a&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;n&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;d in &lt;/span&gt;&lt;span class="ContextualSpellingAndGrammarError SCXW24164227 BCX8"&gt;a&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt; area of rough knobby terrain along the west edge of the quadrangle. The central plains descend northward into the circumpolar lowlands (Arcadia Plan&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt;itia, &lt;/span&gt;&lt;span class="SpellingError SCXW24164227 BCX8"&gt;Vastitas&lt;/span&gt;&lt;span class="NormalTextRun SCXW24164227 BCX8"&gt; Borealis) and rise southward where they are bounded by the cratered terrains of the equatorial region of Mars.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i1049</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Geologic map of the Amazonis Quadrangle of Mars</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>