R.L. Baum, S.R. Spengler, J.D. Torikai, L.A. Liu
1990, Open-File Report 90-531
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Page 476, results 11876 - 11900
Publication Extents
Not all publications have extents, not all extents are completely accurateM. J. Kleeschulte, P. W. Cross
1990, Open-File Report 90-552
No abstract available....
1990, Open-File Report 90-583
Water resources activities of the U.S. Geological Survey in Iowa consist of collecting hydrologic data and conducting interpretive studies. Hydrologic investigations in Iowa are made through three basic types of projects: (1) hydrologic data-collection programs; (2) local or areal hydrologic studies; and (3) statewide or regional investigations. These projects are...
Kenneth L. Wahl, Alberto Condes de la Torre, Frederick A. Kilpatrick, Lawrence A. Martens, Harold C. Mattraw, David W. Pollock, Joseph S. Rosenshein, Wayne B. Solley
1990, Open-File Report 90-184
D. J. Fitzpatrick, P.W. Westerfield
1990, Open-File Report 89-623
An abandoned barite mine in Hot Spring County, Arkansas, has been selected as the location for a proposed gamma-ray and neutrino detector site. As part of the hydrologic evaluation of the site, the U.S. Geological Survey in cooperation with the Arkansas Geological Commission collected hydrologic data at selected locations in...
J.L. Fio, S. J. Deverel
1990, Open-File Report 90-137
Ground-water-flow modeling was used to estimate ground-water-flow paths and traveltimes to quantitatively assess the hydrologic processes affecting ground water and solute movement to drain laterals. Modeling results were used to calculate the depth distribution of ground water flowing into drain laterals at 1.8 meters (drain lateral 1) and 2.7 meters...
K.E. Goddard, editor(s)
1990, Open-File Report 89-580
The Cheyenne River System in western South Dakota has been impacted by the discharge of about 100 million metric tons of gold-mill tailings to Whitewood Creek near Lead, South Dakota. In April 1985, the U.S. Geological Survey initiated an extensive series of research studies to investigate the magnitude of the...
R.F. Duwelius
1990, Open-File Report 90-159
Water resources are abundant in Marion County, Indiana, and have been developed for public and industrial supply, energy generation, irrigation, and recreation. The largest water withdrawals are from surface water, and the two largest water uses are public supply and cooling water for electrical-generating plants. Water-resources programs in the county...
Jeffrey D. Martin, Charles G. Crawford, Richard F. Duwelius, Danny E. Renn
1990, Water Supply Paper 2368-A
This report describes the physical and human environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds selected for study of the hydrologic effects of surface coal mining. The report summarizes information on the geology, geomorphology, soils, climate, hydrology, water use, land use, population, and coal-mining history...
Jeffrey D. Martin, Richard F. Duwelius, Charles G. Crawford
1990, Water Supply Paper 2368-B
Six small watersheds in west-central Indiana were selected for study of the hydrologic effects of surface coal mining and reclamation. The watersheds include mined and reclaimed, mined and unreclaimed, and unmined agricultural land uses and are each less than 3 square miles in area. Surface-water, ground-water, and meteorologic data for...
S. J. Deverel, J.L. Fio
1990, Open-File Report 90-136
A study was undertaken to quantitatively evaluate the hydrologic processes affecting the chemical and isotopic composition of drain-lateral water in a drained agricultural field in the western San Joaquin Valley, California. The results of chemical and isotopic analysis of the samples and analysis of hydraulic-head data and drain-lateral flow data...
L.C. Davis, J. R. Pittman
1990, Open-File Report 90-114
J.B. Czarnecki
1990, Open-File Report 89-595
Alberto Condes de la Torre
1990, Open-File Report 90-171
Scott C. Christenson, David L. Parkhurst, Roy W. Fairchild
1990, Open-File Report 90-570
The Roubidoux aquifer is an important source of freshwater for public supplies, commerce, industry, and rural water districts in northeastern Oklahoma. Ground-water withdrawals from the aquifer in 1981 were estimated to be 4.8 million gallons per day, of which about 90 percent was withdrawn in Ottawa County. Wells drilled at...
E. F. Bugliosi
1990, Open-File Report 90-151
The major aquifers of 35,000 sq mi area in western Ohio and eastern Indiana consist of Silurian and Devonian carbonate bedrock and Quaternary glacial deposits. These bedrock units and glacial deposits have been designated for study as part of the U.S. Geological Survey 's Regional Aquifer System Analysis program, a...
J. G. Brown
1990, Open-File Report 90-395
M. S. Bedinger, K. A. Sargent, William H. Langer, editor(s)
1990, Professional Paper 1370-G
The Bonneville region of the Basin and Range province in westcentral Utah and adjacent Nevada includes several basins lying south of the Great Salt Lake Desert. Physiographically, the region consists of linear, north-trending mountain ranges separated by valleys, many of which are closed basins underlain by thick sequences of fill....
C. H. Tibbals
1990, Professional Paper 1403-E
No abstract available....
A.B. Hoos
1990, Water-Resources Investigations Report 90-4015
Quantitative information concerning aquifer hydrologic and hydraulic characteristics is needed to manage the development of ground-water resources. These characteristics are poorly defined for the bedrock aquifers in Middle and East Tennessee where demand for water is increasing. This report presents estimates of recharge rate, storage coefficient, diffusivity, and transmissivity for...
G.D. Bennett, T. E. Reilly, M. C. Hill
1990, Water-Resources Investigations Report 89-4134
B. H. Ringen, P. B. Daddow
1990, Water-Resources Investigations Report 89-4002
The potential for developing water supplies from the alluvium along the Powder River between Sussex, Wyoming, and Moorehead, Montana, is very limited. The areal extent and saturated thickness of the alluvium are not large. Water in the alluvium primarily is derived from seepage from the river, which goes dry periodically....
W. G. Wright
1990, Water-Resources Investigations Report 90-4134
R. A. Sloto
1990, Water-Resources Investigations Report 89-4169
Sixty-eight percent of the 22.6-square-mile Valley Creek basin is underlain by Cambrian and Ordovician limestone and dolomite. Ground water flows through a network of interconnected secondary openings; primary porosity is virtually nonexistent. Some of these openings have been enlarged by solution. Secondary porosity and permeability exhibit great spatial variability, and...
R. G. Garrett
1990, Water-Resources Investigations Report 90-4097
Falls Lake, an 11,300-acre reservoir in the north-central Piedmont of North Carolina, was completed in December 1983. Hydrologic data were collected at seven inflow sites and one outflow site between 1982 and 1987 to define water-quality characteristics. Data include streamflow data and 56 physical and chemical characteristics of streamwater. Concentrations...