Pg. 28, 74-76. Dewitt formation. All lacustrine and littoral sediments deposited on Coastal Plain of Texas during Miocene and early Pliocene time. Cross-bedded, coarse, gray, semi-indurated, highly calcareous sandstones, with lenses of clay in places. Thickness 1,250 to 1,500 feet. Seaward the time equivalent is represented by marine sands and clays, but these are not included in Dewitt formation. Unconformably underlies Uvalde formation and overlies Fleming clay.
[Named from Dewitt Co., eastern TX.]
Source: US geologic names lexicon (USGS Bull. 896, p. 606).
Dewitt formation. In USGS Prof. Paper 126, 1924, footnotes on p. 97 and 100, is statement that Dewitt formation of USGS Water Supply Paper 335 included Oakville, Lapara, and Lagarto formations.
Source: US geologic names lexicon (USGS Bull. 896, p. 606).
GNC Staff, 1967, [U.S. Geologic Names Committee remarks]: U.S. Geological Survey Bulletin, 1294-A, 55 p.
Dewitt Formation (Miocene and Pliocene) of eastern Texas abandoned. Formation was named by Deussen (1914). In subsequent work by Deussen the name was not used nor was it ever used by any other author. Abandoned for nonuse.
Source: Changes in stratigraphic nomenclature, 1968 (USGS Bull. 1294-A, p. A6.)
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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