Age and movement of ground water in the Madison Limestone, northeastern Wyoming
The Madison Limestone forms a highly productive aquifer in the Powder River basin, Wyoming. The Madison in the study area is a highly fractured limestone, 90 to 200 m thick, with significant percentages of dolomite. Study of Madison water quality in Weston and Crook Counties, Wyoming indicated rapid...
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| Language: | en |
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The University of Arizona.
1981
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| Online Access: | http://hdl.handle.net/10150/191735 http://arizona.openrepository.com/arizona/handle/10150/191735 |