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Tallahatta formation and Neshoba sand

Tallahatta formation and Neshoba sand - (Claiborne group), Southeast of Pearl River predominantly more or less glauconitic claystone and clay with lenses of sand and some sandstone; highly cross-bedded sand at base; northwest of Pearl river predominantly sand, locally glauconitic, containing claystone and clay lenses and abundant clay stringers; Neshoba sand, sparingly glauconitic fairly coarse sand not recognized southeast of Newton County or north of Yalobusha River.
StateMississippi
NameTallahatta formation and Neshoba sand
Geologic ageEocene
Original map labelEt
CommentsSecondary unit descriptions from USGS Lexicon website (MS002) and MS004: Tallahatta Formation of Claiborne Group in Newton Co., MS, divided into lower Basic City Shale Member and upper Neshoba Sand Member. Neshoba is not encountered at the surface in Clarke Co., and is not considered a separate geologic unit in Lauderdale Co. Unit as exposed in study area is typically moderate- to dark reddish-brown, coarse- to fine-grained, consistently micaceous, locally glauconitic, massive, nonfossiliferous sand. Usually has mottled appearance. In the subsurface, it is typically grayish-orange, very coarse- to fine-grained, poorly sorted, subangular quartz sand, with appreciable glauconite and mica. Generally 10 ft thick; 15 ft in Test Hole A0-9. Contact with Basic City Shale Member is conformable. Upper contact with Winona Formation is disconformable. Represents a coarsening upward sequence of sediments produced as the sea regressed in a deltaic and strandplain environment. Measured section. Geologic map. Stratigraphic column (Merrill and others, 1985).
Primary rock typeclaystone
Secondary rock typeclay or mud
Other rock typessand; sandstone
Lithologic constituents
Major
Unconsolidated > Fine-detrital > Clay (Bed)Southeast of Pearl River predominantly more or less glauconitic claystone and clay with lenses of sand and some sandstone; highly cross-bedded sand at base.
Sedimentary > Clastic > Mudstone > Claystone (Bed)Southeast of Pearl River predominantly more or less glauconitic claystone and clay with lenses of sand and some sandstone; highly cross-bedded sand at base.
Minor
Sedimentary > Clastic > Sandstone (Lense)Southeast of Pearl River predominantly more or less glauconitic claystone and clay with lenses of sand and some sandstone; highly cross-bedded sand at base.
Unconsolidated > Coarse-detrital > Sand (Bed)Southeast of Pearl River predominantly more or less glauconitic claystone and clay with lenses of sand and some sandstone; highly cross-bedded sand at base.
Map references
Moore, William Halsell, 1969, reprinted 1985, Geologic Map of Mississippi, Compiled by Bicker, A. R., Jr., a revision of the geologic map published by the MS Geological Survey in 1945 in cooperation with the USGS, revised from data submitted by Dr. E. E. Russell of MS State University from published reports of the MS Geological Survey and from field revisions, Mercury Maps Inc., Jackson, MS.
Unit references
Moore, William Halsell, 1969, reprinted 1985, Geologic Map of Mississippi, Compiled by Bicker, A. R., Jr., a revision of the geologic map published by the MS Geological Survey in 1945 in cooperation with the USGS, revised from data submitted by Dr. E. E. Russell of MS State University from published reports of the MS Geological Survey and from field revisions, Mercury Maps Inc., Jackson, MS.
USGS Geologic Names Lexicon (GEOLEX)
Merrill, R.K., Sims, J.J., Jr., Gann, D.E. and Liles, K.J., 1985, Newton County geology and mineral resources [Mississippi]: Mississippi Office of Geology Bulletin, no. 126, 108 p.
Geographic coverageAttala - Benton - Calhoun - Carroll - Choctaw - Clarke - DeSoto - Grenada - Lafayette - Lauderdale - Leake - Marshall - Montgomery - Neshoba - Newton - Panola - Tallahatchie - Tate - Tippah - Winston - Yalobusha

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