Uranium-Bearing Sandstone in the White River Badlands, Pennington County, South Dakota

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Description

From abstract: The uranium mineral uranocircite, a barium uranyl phosphate, occurs in a sandstone channel in the Chadron formation of Oligocene age in the White River Badlands, Pennington County, S. Dak. A vertical section of the basal 1-foot of the channel contains 0. 25 percent uranium. There are also small amounts of metatyuyamunite (?) in the upper part of a freshwater lime stone bed in the Chadron formation and carnotite in chalcedony veins in the overlying Brule formation, also of Oligocene age.

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24 p. : ill., maps ; 28 cm.

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Moore, George W. & Levish, Murray April 1954.

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From abstract: The uranium mineral uranocircite, a barium uranyl phosphate, occurs in a sandstone channel in the Chadron formation of Oligocene age in the White River Badlands, Pennington County, S. Dak. A vertical section of the basal 1-foot of the channel contains 0. 25 percent uranium. There are also small amounts of metatyuyamunite (?) in the upper part of a freshwater lime stone bed in the Chadron formation and carnotite in chalcedony veins in the overlying Brule formation, also of Oligocene age.

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24 p. : ill., maps ; 28 cm.

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  • April 1954

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  • Jan. 27, 2017, 10:19 a.m.

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  • Jan. 2, 2018, 6:39 p.m.

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Moore, George W. & Levish, Murray. Uranium-Bearing Sandstone in the White River Badlands, Pennington County, South Dakota, report, April 1954; Washington D.C. (https://digital.library.unt.edu/ark:/67531/metadc304587/: accessed March 28, 2025), University of North Texas Libraries, UNT Digital Library, https://digital.library.unt.edu; crediting UNT Libraries Government Documents Department.

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