<?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>Richard S. Moreland</dc:contributor>
  <dc:contributor>Amy E. Clark</dc:contributor>
  <dc:creator>James L. Robinson</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>Baldwin County, the fastest growing county in Alabama in 1995, is 100-percent dependent on ground water for public water supply. Ground-water withdrawals in Baldwin County were estimated to be about 7 million gallons per day in 1996, 12 million gallons per day in 1980, and 30 gallons per day in 1990. The effects of future increases in ground-water withdrawals, to supply the needs of the growing county population, cannot be assessed without defining baseline conditions. To address the future of ground-water development, the Baldwin County Commission requested the USGS to perform a study of the ground-water resources of Baldwin County.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr96590</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Potentiometric surface of the Miocene-Pliocene aquifer system of Baldwin County, Alabama, 1995</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>