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Results for “Energies”
Search indexed USGS publications on groundwater, aquifers, geologic maps, mineral resources and earthquakes. Explore source records by subject and place.
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Proceedings of the Illinois Basin energy and mineral resources workshop
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Enthalpy and Gibbs energy of formation of dolomite, CaMg(CO 3 ) 2 , at 298.15 K from HCl solution calorimetry
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The future of energy gases
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Bibliography of publications by members of the Branch of Coal Geology, Office of Energy and Marine Geology, U.S. Geological Survey, January 1, 1985-September 30, 1994
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Bibliography of publications by members of the Branch of Coal Geology, Office of Energy and Marine Geology, U.S. Geological Survey, January 1, 1985-September 30, 1994
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Energy and mineral resource assessment of the Ashland Division of the Custer National Forest, Powder River and Rosebud Counties, southeastern Montana
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Bibliography of papers on natural gas written by U.S. Geological Survey, Energy Resource Surveys Authors, 1990-1995
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Mineral and energy resource assessment of the Helena National Forest, west-central Montana
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Digital maps and figures on CD-ROM for Mineral and energy resource assessment of the Helena National Forest, west-central Montana
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Geology, mineral and energy resources, Mimbres Resource Area, New Mexico
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Preliminary report on the International Energy Agency mode of occurrence inter-laboratory comparison; Phase I, USGS results
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Demand and supply of nonfuel minerals and materials for the United States energy industry, 1975-1990 :a preliminary report
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Geology and energy resources of the Sand Butte Rim NW quadrangle, Sweetwater County, Wyoming
The Sand Butte Rim NW 71-minute quadrangle occupies 56 square miles of an arid, windy, sparsely vegetated area of ridges and valleys on the east flank of the Rock Springs uplift in southwest Wyoming. The area is underlain by a succession of sedimentary rocks, about 20,000 feet thick, that includes 28 formations ranging in age from Cambrian to Tertiary. Upper Cretaceous and lower Tertiary formations crop out and dip 3?-6? southeast. They are unfaulted and generally homoclinal, but a minor anticlinal nose is present. Older rocks in the subsurface are faulted and folded. Coal resources are estimated to be nearly I billion short tons of subbituminous coal, in beds more than 2.5 feet thick, under less than 3,000 feet of overburden, in the Fort Union Formation of Paleocene age and the Lance and Almond Formations of Cretaceous age.
Geochemistry of some rocks, mine spoils, stream sediments, soils, plants, and waters in the Western Energy Region of the conterminous United States, with sections on field studies
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The future of energy gases
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