<?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>William Jasper Sando</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>&lt;p&gt;The name Crummies Member of the Breathitt Formation is here given to a marine unit that I.C. White in 1885&amp;nbsp;called the Cannelton Limestone in the Kanawha River&amp;nbsp;valley of West Virginia. Rocks now assigned to the Crummies Member have been miscorrelated by other workers&amp;nbsp;with the Campbell Creek Limestone of White (1885) in&amp;nbsp;other areas of West Virginia as well as in eastern Kentucky&amp;nbsp;and southwestern Virginia. Fieldwork and literature review&amp;nbsp;suggest that the Crummies Member is an extensive deposit.&amp;nbsp;In southeasternmost Kentucky, where it contains a varied&amp;nbsp;molluscan fauna, it attains its greatest thickness; in northeastern Kentucky, it is present as a thin, discontinuous&amp;nbsp;sandstone and sandy siltstone unit that contains more openmarine fauna. &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/b2073</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Government Printing Office</dc:publisher>
  <dc:title>Shorter contributions to paleontology and stratigraphy, 1993</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>