<?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>John G. Newton</dc:creator>
  <dc:date>1979</dc:date>
  <dc:description>&lt;p&gt;Test wells in Dallas and Sumter counties, Alabama penetrated deep Cretaceous aquifers that are sources of future ground-water withdrawals. The test well in Dallas County was drilled to a depth of 1,460 feet, and the test well in Sumter County was drilled to a depth of 2,311 feet. The deep aquifers in Sumter County are in an area of future residential and industrial development along the Tennessee-Tombigbee Waterway. Descriptions of drill cuttings are given in the report.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr791485</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Sample descriptions for test wells penetrating deep aquifers in Dallas and Sumpter counties, Alabama</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>