2 edition of Geologic environment of an oxidized uranium deposit in the Black Hills, South Dakota found in the catalog.
Geologic environment of an oxidized uranium deposit in the Black Hills, South Dakota
Norman P. Cuppels
Published
1962
by U.S. Govt. Print. Off. in Washington
.
Written in English
Edition Notes
| Statement | by N. P. Cuppels ; prepared on behalf of the U.S. Atomic Energy Commission and published with the permission of the Commission. |
| Series | Geological Survey bulletin -- 1063-C, Geology and uranium deposits in southern Black Hills, Geology and uranium deposits of the southern Black Hills |
| Contributions | U.S. Atomic Energy Commission. |
| The Physical Object | |
|---|---|
| Pagination | iv, 61-83 p. : |
| Number of Pages | 83 |
| ID Numbers | |
| Open Library | OL22971868M |
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The caves of the Black Hills are located in Carboniferous limestone and dolomite of the Madison Formation in western South Dakota. The climate is semi-arid, and surface karst features are few.
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Geologic environment of an oxidized uranium deposit in the black hills South Dakota / N. Cuppels N.P. Cuppels Geology and uranium deposits of the. Examples of this deposit type can be found around the world, but in Australia the biggest one is the Mary Kathleen uranium-rare earths deposit near Mount Isa.
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