<?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>R. A. De Hon</dc:creator>
  <dc:date>1992</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="TextRun SCXW161557503 BCX8" lang="EN-US" xml:lang="EN-US" data-contrast="auto"&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;The Pompeii quadrangle is in the northern Maja Valles between &lt;/span&gt;&lt;span class="SpellingError SCXW161557503 BCX8"&gt;Lunae&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt; Planum to the west and &lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;Xanthe&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt; Terra to the east (fig. 1). &lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;Approximately&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt; two-thirds of the surface is relatively smooth plains, and the other &lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;one-third is subdued, cratered, upland plateau. Several large (greater than 30 km in diameter) craters dominate the landscape. The crater Pompeii is the largest fresh crater in the quadrangle. The major interes&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;t in the map area is evidence of the relatively brief, catastrophic Maja outflow and its associated&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt; topographic modification of much of the area. The effects of erosion and deposition by the Maja flood are pronounced and are a chief &lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt;part of the story; therefore, flood-modified terrain is divided in considerable detail.&lt;/span&gt;&lt;span class="NormalTextRun SCXW161557503 BCX8"&gt; The stratigraphic units associated with the outflow are true rock units although they may be very thin.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i2203</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Geologic map of the Pompeii Quadrangle (MTM 20057), Maja Valles region of Mars</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>