<?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>Thomas G. Gibson</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>The only semipermanent surface water available on the Southern High &#13;
Plains plateau of Texas and New Mexico is contained in saline lakes and &#13;
in the playa lakes that form in shallow depressions, called playa &#13;
basins, following heavy rainfall. The playas generally are accepted as &#13;
the main source of recharge to the underlying High Plains (Ogallala) &#13;
aquifer of the region, and they constitute the major wildlife habitat on &#13;
the Southern High Plains. Their use as water sources, holding ponds, &#13;
and waste-disposal sites by agricultural and industrial operations may &#13;
potentially lead to ground-water contamination and habitat degradation.  &#13;
Therefore, playa lakes will play an essential role in the collection of &#13;
surface-water quality and ecological data for the Southern High Plains &#13;
study unit of the National Water-Quality Assessment program of the U.S. &#13;
Geological Survey.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr94702</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey,</dc:publisher>
  <dc:title>Neogene and Quaternary foraminifera and paleoenvironments of a corehole from Horn Island, Mississippi</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>