Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area
M.L. Sorey, S. E. Ingebritsen
1984, Water-Resources Investigations Report 84-4278
The conceptual model of the Lassen system is termed a liquid-dominated hydrothermal system with a parasitic vapor-dominated zone. The essential feature of this model is that steam and steam-heated discharge at relatively high elevations in Lassen Volcanic National Park (LVNP) and liquid discharge with high chloride concentrations at relatively low...
Maps showing altitude of the potentiometric surface and changes in water levels of the alluvial aquifer in eastern Arkansas, Spring 1983
Joe Edds, Daniel J. Fitzpatrick
1984, Water-Resources Investigations Report 84-4264
The Mississippi River Alluvial Aquifer is a major source of water supply for irrigation in much of eastern Arkansas. Hydrologic maps of the potentiometric surface, water-level changes and depths to water in the aquifer, based on Spring 1983 measurements, are presented. The Mississippi River Alluvial Aquifer is comprised of Quaternary...
Water-data program of the US Geological Survey in Kansas, fiscal year 1983
R.K. Livingston, K.D. Medina
1984, Water-Resources Investigations Report 84-4306
The U.S. Geological Survey is the principal Federal agency responsible for the collection of hydrologic data needed for the planning, development, use, and management of the water resources in Kansas. Hydrologic-data collection by the U.S. Geological Survey in Kansas began in 1895. The fiscal-year 1983 water-data program, operated in cooperation...
Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky
Samuel S. Leung, D.W. Leist, R. W. Davis, Steven Cordiviola
1984, Water-Resources Investigations Report 84-4073
Oil shales in Kentucky are rocks of predominantly Devonian age. The most prominant are the Ohio, Chattanooga, and New Albany Shales. A leaching study was done on six fresh oil shale samples and one retorted oil shale sample. Leaching reagents were distilled water, 0.0005 N sulfuric acid, and 0.05 N...
Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada
R. W. Craig, J. H. Robison
1984, Water-Resources Investigations Report 84-4248
Test well UE-25pNo1 was drilled in cooperation with the U.S. Department of Energy in the southwestern part of the Nevada Test Site, for investigations related to the isolation of high-level nuclear wastes. Rocks penetrated in the well are predominantly ash-flow tuffs of Tertiary age to a depth of 1,244 meters...
Hydrology and land use in Van Buren County, Michigan
T. R. Cummings, F. R. Twenter, D. J. Holtschlag
1984, Water-Resources Investigations Report 84-4112
This report gives the results of an investigation to determine the chemical and physical characteristics of ground and surface water in Van Buren County and to relate these characteristics to the agricultural use of land. Chemical inputs to the hydrologic system, including those from precipitation, animal wastes, septic tanks, and...
Finite-element simulation of ground-water flow in the vicinity of Yucca Mountain, Nevada-California
J.B. Czarnecki, R. K. Waddell
1984, Water-Resources Investigations Report 84-4349
A finite-element model of the groundwater flow system in the vicinity of Yucca Mountain at the Nevada Test Site was developed using parameter estimation techniques. The model simulated steady-state ground-water flow occurring in tuffaceous, volcanic , and carbonate rocks, and alluvial aquifers. Hydraulic gradients in the modeled area range from...
Map showing outcrops of granitic rocks, Basin and Range Province, Nevada
K. A. Sargent, Kurt Roggensack
1984, Water-Resources Investigations Report 83-4119-D
This map report is one of a series of geologic and hydrologic maps covering all or parts of States within the Basin and Range province of the western United States. The map reports contain information on subjects that characterize the geohydrology of the province, including the ground-water hydrology, ground-water quality,...
Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Oregon
Thomas H. Thompson, Richard Chappell, J. B. Gonthier, W. D. McFarland
1984, Water-Resources Investigations Report 83-4120-C
This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural...
Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Southern California
Thomas H. Thompson, Janet Nuter, W. R. Moyle Jr., Linda R. Woolfenden
1984, Water-Resources Investigations Report 83-4116-C
This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural...
Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon
J.E. Reed, M. S. Bedinger, J. B. Gonthier, William H. Langer, W. D. McFarland, D. A. Mulvihill
1984, Water-Resources Investigations Report 83-4120-B
This report on ground-water levels, springs and depth to ground water in the Basin and Range province of Oregon (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high level nuclear waste (Bedinger,...
Hydrologic, demographic, and land-use data for the Snake River Plain, southeastern Idaho
H.W. Young, Michael L. Jones
1984, Water-Resources Investigations Report 84-4001
No abstract available. ...
Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California
William H. Langer, W. R. Moyle, L. R. Woolfenden, D. A. Mulvihill
1984, Water-Resources Investigations Report 83-4116-B
This report on ground-water levels, springs and depth to ground water in the Basin and Range province of southern California (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent,...
Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas
B. T. Brady, M. S. Bedinger, D. A. Mulvihill, John Mikels, W. H. Langer
1984, Water-Resources Investigations Report 83-4121-B
This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Texas (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent,...
Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Nevada
M. S. Bedinger, J. R. Harrill, William H. Langer, J. M. Thomas, D. A. Mulvihill
1984, Water-Resources Investigations Report 83-4119-B
This report on ground-water levels, springs and depth to ground water in the Basin and Range province of Nevada (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent,...
Maps showing ground-water levels, springs, and depth to ground water, Basin and Range province, Utah
M. S. Bedinger, J. L. Mason, W. H. Langer, J. S. Gates, J. R. Stark, D. A. Mulvihill
1984, Water-Resources Investigations Report 83-4122-B
This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Utah (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent,...
Evaluation of hydrologic processes affecting soil movement in the Hagerman fauna area, Hagerman, Idaho
H.W. Young
1984, Water-Resources Investigations Report 84-4137
The Hagerman fauna area on the western slope of the Snake River canyon in south-central Idaho is one of the most important locations of upper Pliocene fossils in the world. The fossil beds are distributed vertically through a 500-foot stratigraphic section of the Glenns Ferry Formation. Accelerated soil movement caused...
Estimation of streamflow for selected sites on the Carson and Truckee rivers in California and Nevada, 1944-80
J. C. Blodgett, R.N. Oltmann, K.R. Poeschel
1984, Water-Resources Investigations Report 84-4058
Daily mean and monthly discharges were estimated for 10 sites on the Carson and Truckee Rivers for periods of incomplete records and for tributary sites affected by reservoir regulation. On the basis of the hydrologic characteristics, stream-flow data for a water year were grouped by month or season for subsequent...
Ground water hydrology of the Elizabethtown area, Kentucky
D. S. Mull, M. A. Lyverse
1984, Water-Resources Investigations Report 84-4057
The principal aquifer in a 52 square mile karst area in north central Kentucky is the St. Louis Limestone of Mississippian age. Unconsolidated residuum and surficial deposits of slumped material may store water and recharge the underlying limestone aquifer. Precipitation averages 49 inches annually; 6 inches recharges ground-water reservoirs. The...
Hydrology of Prairie Dog Creek Valley, Norton Dam to state line, north-central Kansas
L.E. Stullken
1984, Water-Resources Investigations Report 84-4162
Development of water resources has been a major factor in the economy of Prairie Dog Creek Valley in north-central Kansas. Releases from Norton Reservoir to the Almena Irrigation District averaged 6,900 acre-feet per year during 1967-76. The number of irrigation wells increased from 4 to 147 during 1947-78. Ground water...
Conceptual hydrologic model of flow in the unsaturated zone, Yucca Mountain, Nevada
P.M. Montazer, W.E. Wilson
1984, Water-Resources Investigations Report 84-4345
The unsaturated volcanic tuffs beneath Yucca Mountain, Nevada, are being evaluated as a host rock for a potential repository for high-level radioactive waste. A conceptual hydrologic model is proposed to describe the flow of fluids through these rocks. Thickness of the unsaturated zone is about 500 to 750 meters and...
Ground water in the Fresno area, California; preliminary report
H. T. Mitten
1984, Water-Resources Investigations Report 83-4246
The U.S. Geological Survey, in cooperation with Fresno County, is developing a computer model of the unconfined aquifer system in the Fresno area. In the area, consolidated rocks are overlain by unconsolidated deposits. The unconsolidated deposits are divided into a lower fine-grained unit and an overlying coarse-grained unit. The system...
Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach
T. L. Miller, J. B. Gonthier
1984, Water-Resources Investigations Report 84-4242
An appraisal of Oregon ground-water quality was made using existing data accessible through the U.S. Geological Survey computer system. The data available for about 1,000 sites were separated by aquifer units and hydrologic units. Selected statistical moments were described for 19 constituents including major ions. About 96 percent of all...
Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama, fiscal year 1983
Fred Morris III
1984, Open-File Report 84-717
Cost effectiveness of the U.S. Geological Survey's stream-gaging program in Illinois
D. M. Mades, K. A. Oberg
1984, Water-Resources Investigations Report 84-4123
Data uses and funding sources were identified for 138 continuous-record discharge-gaging stations currently (1983) operated as part of the stream-gaging program in Illinois. Streamflow data from five of those stations are used only for regional hydrology studies. Most streamflow data are used for defining regional hydrology, defining rainfall-runoff relations, flood...
