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Page 23, results 551 - 575

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Living with volcanoes
Thomas L. Wright, Thomas C. Pierson
1992, Circular 1073
The 1980 cataclysmic eruption of Mount St. Helens (Lipman and Mullineaux, 1981) in southwestern Washington ushered in a decade marked by more worldwide volcanic disasters and crises than any other in recorded history. Volcanoes killed more people (over 28,500) in the 1980's than during the 78 years following 1902 eruption...
The Alaska Mineral Resource Assessment Program: Background information to accompany geologic and mineral-resource maps of the Cordova and Middleton Island quadrangles, southern Alaska
Gary R. Winkler, George Plafker, R.J. Goldfarb, J. E. Case
1992, Circular 1076
This report summarizes recent results of integrated geological, geochemical, and geophysical field and laboratory studies conducted by the U.S. Geological Survey in the Cordova and Middleton Island 1°x3° quadrangles of coastal southern Alaska. Published open-file reports and maps accompanied by descriptive and interpretative texts, tables, diagrams, and pertinent references provide...
The Conterminous United States Mineral Assessment Program: Background information to accompany folio of geologic, geochemical, geophysical, and mineral resource maps of the Ajo and Lukeville 1° by 2° quadrangles, Arizona
Floyd Gray, R. M. Tosdal, J.A. Peterson, D. P. Cox, R. J. Miller, D. P. Klein, P. K. Theobald, G. B. Haxel, M. J. Grubensky, G. L. Raines, H. N. Barton, D.A. Singer, R. G. Eppinger
1992, Circular 1082
Encompassing about 21,000 km2 in southwestern Arizona, the Ajo and Lukeville 1° by 2°  quadrangles have been the subject of mineral resource investigations utilizing field and laboratory studies in the disciplines of geology, geochemistry, geophysics, and Landsat imagery. The results of these studies are published as a folio of maps,...
The Conterminous United States Mineral Assessment Project; background information to accompany folio of geologic, geochemical, geophysical, and mineral resources maps of the Reno 1 by 2 degree Quadrangle, Nevada and California
David A. John, John H. Stewart, J. D. Hendricks, L. C. Rowan, Donald Plouff
1992, Circular 1078
The Reno 1 ? by 2 ? quadrangle in west-central Nevada was studied by an interdisciplinary research team to appraise its mineral resources. The assessment is based on geological, geochemical, and geophysical field and laboratory investigations, the results of which are published as a folio of maps, reports, figures, and...
The Conterminous United States Mineral Appraisal Program; background information to accompany folio of geologic, geochemical, geophysical, and mineral resources maps of the Tonopah 1 by 2 degree Quadrangle, Nevada
David A. John, J. T. Nash, Donald Plouff, D. H. Whitebread
1991, Circular 1070
The Tonopah 1 ? by 2 ? quadrangle in south-central Nevada was studied by an interdisciplinary research team to appraise its mineral resources. The appraisal is based on geological, geochemical, and geophysical field and laboratory investigations, the results of which are published as a folio of maps, figures, and tables,...
Economic effects of western Federal land-use restrictions on U.S. coal markets
William Downing Watson, A.L. Medlin, K.K. Krohn, D.S. Brookshire, R. L. Bernknopf
1991, Circular 1042
Current regulations on land use in the Western United States affect access to surface minable coal resources. This U.S. Geological Survey study analyzes the long-term effects of Federal land-use restrictions on the national cost of meeting future coal demands. The analysis covers 45 years. The U.S. Bureau of Land Management...
Hydrology of the Arbuckle Mountains area, south-central Oklahoma
Roy W. Fairchild, Ronald L. Hanson, Robert E. Davis
1990, Circular 91
Rocks that make up the Arbuckle-Simpson aquifer crop out over ~500 mi2 in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000-9,000 ft thick. The rocks were...
Coasts in crisis
S. Jeffress Williams, Kurt A. Dodd, Kathleen K. Gohn
1990, Circular 1075