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<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>Walter C. Warren</dc:contributor>
  <dc:contributor>Raymond M. Thompson</dc:contributor>
  <dc:contributor>Elizabeth F. Overstreet</dc:contributor>
  <dc:creator>Walter B. Lang</dc:creator>
  <dc:date>1965</dc:date>
  <dc:description>The Irwinton district is in the central part of Georgia at the inner margin &#13;
of the Coastal Plain province. The oldest rocks exposed in the district are &#13;
crystalline rocks of the Piedmont province. They are unconformably overlain &#13;
by nonmarine sedimentary strata of Late Cretaceous age, including gravel, &#13;
micaceous sand, and lenses of kaolin.&#13;
&#13;
Bauxite has been found in a few of the kaolin lenses near the top of the &#13;
sequence of these strata. During a long period prior to deposition of the over- &#13;
lying marine beds of the Claiborne and Jackson Groups (middle and upper &#13;
Eocene), the Upper Cretaceous strata were subjected to subaerial erosion. &#13;
The bauxite deposits are considered to have formed during this period. They &#13;
range in thickness from a few inches to more than 10 feet and occupy areas &#13;
ranging from a few square feet to more than 5 acres. Most of the known &#13;
bauxite deposits lie along the valleys of Commissioners Creek and Big Sandy &#13;
Creek in Wilkinson County. The kaolin lenses are much larger than the &#13;
bauxite deposits; some of the lenses underlie more than 200 acres and are &#13;
more than 20 feet thick.&#13;
&#13;
Bauxite was discovered in the district in 1907 and was mined from 1910 to &#13;
1928. A few additional carloads of ore were shipped in 1941 and 1942, but &#13;
no ore has been mined since that time. Reserves of high-grade bauxite are &#13;
very small. Reserves of all grades of bauxite plus bauxitic clay may be about &#13;
400,000 long tons.&#13;
&#13;
The Irwinton district is the principal source of high-grade kaolin in the &#13;
United States. The presence of kaolin here has been known since early colo- &#13;
nial time, and it has been mined continuously since 1897. Production in 1959 &#13;
was 1,940,279 short tons. The reserves of kaolin are very large but have never &#13;
been adequately measured. Reserves of first and second grade kaolin may be &#13;
67 to 84 million short tons. Kaolin of lower grade is present in larger quantity.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/b1199J</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Bauxite and Kaolin Deposits of the Irwinton district, Georgia</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>