John B. Townshend, J.E. Papp, H.K. Rex, L.Y. Torrence, P.A. Franklin
1986, Open-File Report 86-300-A
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Page 1541, results 38501 - 38525
Publication Extents
Not all publications have extents, not all extents are completely accurateAlan H. Welch, Rhea P. Williams
1986, Open-File Report 85-648-B
Water quality data for groundwater were compiled for the Elko 1 degree x 2 degree quadrangle which covers a portion of Eastern Nevada. Chemical characteristics of the water are shown on a map (at a scale of 1:250,000) and on trilinear diagrams for the major ions. The data for the...
Alan H. Welch, Rhea P. Williams
1986, Open-File Report 85-648-C
Water quality data for groundwater were compiled for the Ely 1 degree x 2 degree quadrangle which covers a portion of eastern Nevada. Chemical characteristics of the water are shown on a map (at a scale of 1:250,000) and on trilinear diagrams for the major ions. The data for the...
Joe Edds, D. J. Fitzpatrick
1986, Water-Resources Investigations Report 86-4084
Aquifers in the Tertiary Sparta and Memphis Sands are a major source of water supply for much of eastern and south-central Arkansas. Major withdrawals occur from the aquifer for industrial and public supply, with generally lesser but locally significant amounts withdrawn for agricultural uses. Water level data from wells tapping...
David M. Sutphin, Norman J. Page
1986, Circular 930-E
Major world resources of platinum-group metals are described in this summary report of information in the International Strategic Minerals Inventory {ISMI}. ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, and the United States of...
J. V. Brahana, Mike Bradley, Jo Ann Macy, Dolores Mulderink
1986, Water-Resources Investigations Report 82-762
The basal sandstone is a poorly sorted, well indurated sandstone, which lies below the Conasauga Group and above the Precambrian crystalline rocks. It is an unknown resource defined by limited data, with only 14 data points (wells) for the entire State of Tennessee. The basal sandstone is thought to occur...
Kim-Marie Walker, James York, Dennis Murphy, C. E. Sloan
1986, Water-Resources Investigations Report 86-4143
The National Mapping Division and Water Resources Division of the U.S. Geological Survey have produced a digital data base of approximately 23,330 lakes on the North Slope of Alaska. The inventoried region consists of the area north of the 69th parallel and is composed of sixteen 1° x 3° quadrangles....
Harold Moellering, editor(s)
1986, Open-File Report 87-307
J. K. Odum
1986, Open-File Report 86-382
R. M. Bloyd, P. B. Daddow, P.R. Jordon, H. W. Lowham
1986, Water-Resources Investigations Report 86-4329
The effects of surface coal mining on the surface- and groundwater systems in a 5,400 sq mi area in the Powder River Basin, Wyoming, that includes 20 major coal mines were evaluated using three approaches: A surface water model, a landscape-stability analysis, and a groundwater model. A surface water model...
M.S. Reid, R.A. Renken, R. L. Wait, W. R. Aucott, R. W. Lee
1986, Water-Resources Investigations Report 86-4102
Two test wells were drilled in Marion County, South Carolina in 1982. Well MRN 77 (Marion 77) was drilled to a depth of 365 ft and was used as an observation well in the Black Creek aquifer and to supply water during drilling of the deeper well. MRN 78 (Marion...
Pierre Lacombe
1986, Water-Resources Investigations Report 86-4051
Seismic-refraction, electric-resistivity sounding, and electromagnetic conductivity techniques were used to determine the geohydrologic framework and extent of groundwater contamination at Picatinny Arsenal in northern New Jersey. The area studied encompasses about 4 sq mi at the southern end of the Arsenal. The bedrock surface beneath the glacial sediments was delineated...
Kathryn M. Scanlon
1986, Open-File Report 86-399
J. V. Brahana, Dolores Mulderink, J. A. Macy, M. W. Bradley
1986, Water-Resources Investigations Report 82-4091
The east Tennessee aquifer system occurs in the Valley and Ridge and the Blue Ridge provinces of Tennessee. These areas are underlain by rocks of Precambrian to Pennsylvanian age which have been structurally deformed and faulted during the Appalachian orogeny. Groundwater in the Valley and Ridge occurs primarily in solution...
F.M. Taylor, M.T. Rosier
1986, Open-File Report 86-320
Groundwater investigations began in West Virginia in 1941. As an aid to development and management of the State 's water resources, the U.S. Geological Survey, in cooperation with the West Virginia Geological and Economic Survey, maintains a network of 31 observation wells throughout the State. Some wells are equipped with...
Arthur C. Tarr, A. M. Rogers
1986, Open-File Report 86-420
E. J. Crompton, J. G. Peters, R. L. Miller, J. A. Stewart, K. J. Banaszak, R. J. Shedlock
1986, Water-Resources Investigations Report 86-4157
The St. Joseph River Basin data-collection network in the St. Joseph River for streamflow, lake, ground water, and climatic stations was reviewed. The network review included only the 1700 sq mi part of the basin in Indiana. The streamflow network includes 11 continuous-record gaging stations and one partial-record station. Based...
D. M. Mann, D.W. Scholl, R. W. Sliter
1986, Open-File Report 86-457
R.L. Stahl, K. K. Fitzgerald, T.E. Richards, P.D. Hayes
1986, Water Data Report IL-85-1
Desiree Stuart-Alexander, Larry N. Smith, Carol N. Healy, Evelyn B. Newman, Robert K. Mark
1986, Open-File Report 86-524-B
K. K. Fitzgerald, P.D. Hayes, T.E. Richards, R.L. Stahl
1986, Water Data Report IL-85-2
Jacob Eugene Gair, Richard Goldsmith, D. L. Daniels, W. R. Griffitts, J. H. DeYoung, M. P. Lee
1986, Circular 944
This Circular and the folio of separately published maps described herein are part of a series of reports compiled under the Conterminous United States Mineral Assessment Program ICUSMAP). The folio on the Charlotte 1 degree ? 2 degree quadrangle, North Carolina and South Carolina, includes (1) a geologic map; (2)...
Julia B. Graf
1986, Water Supply Paper 2269
Twenty-seven measurements of traveltime and longitudinal dispersion in 10 Illinois streams made from 1975 to 1982 provide data needed for estimating traveltime of peak concentration of a conservative solute, traveltime of the leading edge of a solute cloud, peak concentration resulting from injection of a given quantity of solute, and...
Stephen P. Garabedian
1986, Water Supply Paper 2278
A nonlinear, least-squares regression technique for the estimation of ground-water flow model parameters was applied to the regional aquifer underlying the eastern Snake River Plain, Idaho. The technique uses a computer program to simulate two-dimensional, steady-state ground-water flow. Hydrologic data for the 1980 water year were used to calculate recharge...
R. E. Rathbun, D. Y. Tai
1986, Water Supply Paper 2286
Volatilization is a significant process in determining the fate of many organic compounds in streams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by measuring the flux for the...