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Page 5902, results 147526 - 147550

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A summary of the geology and mineral resources of the Paris Plateau-House Rock Valley area, Coconino County, Arizona
Morris W. Green, C. T. Pierson, D. P. Bauer, D.B. Umshler
1977, Open-File Report 77-737
The Paria Plateau-House Rock Valley area of north-central Arizona is located on the southwestern edge Of the Colorado Plateau physiographic province in an area underlain by about 5,000 meters of fossiliferous marine and continental sedimentary rock ranging in age from Precambrian through Quaternary. The area, which lies north of the...
Ground-water levels in Wyoming, 1976
Wilbur C. Ballance, Pamela B. Freudenthal
1977, Open-File Report 77-686
Ground-water levels are measured periodically in a network of about 280 observation wells in Wyoming to record changes in ground-water storage. The areas of water-level observation are mostly where ground water is used in large quantities for irrigation or municipal purposes. This report contains maps showing location of observation wells...
Finite-difference model of two-dimensional, single, and two-phase heat transport in a porous medium - Version I
Charles R. Faust, James W. Mercer
1977, Open-File Report 77-234
Model documentation is presented for a two-dimensional (areal) heat-transport model capable of simulating both water- and vapor-dominated geothermal reservoirs that conform with the assumptions of the model. Finite-difference techniques are used to solve for the dependent variables pressure and enthalpy. The program is designed to simulate time-dependent problems such as...
Computation of backwater and discharge at width constrictions of heavily vegetated flood plains
V.R. Schneider, J.W. Board, B.E. Colson, F.N. Lee, Leroy Druffel
1977, Water-Resources Investigations Report 76-129
The U.S. Geological Survey, cooperated with the Federal Highway Administration and the State Highway Departments of Mississippi, Alabama, and Louisiana, to develop a proposed method for computing backwater and discharge at width constrictions of heavily vegetated flood plains. Data were collected at 20 single opening sites for 31 floods. Flood-plain...