<?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>C.L. Sainsbury</dc:contributor>
  <dc:creator>David Scholl</dc:creator>
  <dc:date>1961</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="ScopusTermHighlight"&gt;A&lt;/span&gt;&lt;span&gt;&amp;nbsp;shallow&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;seavalley&lt;/span&gt;&lt;span&gt;, averaging 6 feet in relief, extends from the mouth of Ogotoruk Creek, northwest Alaska, for 15 miles across the floor of the Chukchi&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Sea&lt;/span&gt;&lt;span&gt;&amp;nbsp;to&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;a&lt;/span&gt;&lt;span&gt;&amp;nbsp;depth of 135 feet. The&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;seavalley&lt;/span&gt;&lt;span&gt;&amp;nbsp;is considered to be&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;a&lt;/span&gt;&lt;span&gt;&amp;nbsp;drowned subaerial valley of Pleistocene age, which was excavated on an eustatically emerged&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;epicontinental&lt;/span&gt;&lt;span&gt;&amp;nbsp;shelf during periods of glacially depressed&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;sea&lt;/span&gt;&lt;span&gt;&amp;nbsp;level.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0016-7606(1961)72[1433:SCASUA]2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Subaerially carved Arctic seavalley under a modern epicontinental sea</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>