David L Berger (Former Employee)
Science and Products
Filter Total Items: 26
Water budget estimates for the 14 hydrographic areas in the middle Humboldt River basin, north-central Nevada
Water budgets were developed for the 14 hydrographic areas in the middle Humboldt River Basin of north-central Nevada. The water budgets include estimates of average annual precipitation, runoff, water yield, ground-water recharge and subsurface flow, and evapotranspiration (ET) determined from recently developed or revised methods. Ground-water pumping is not included in the budget estimates. The
Authors
David L. Berger
Water budgets for Pine Valley, Carico Lake Valley, and Upper Reese River Valley hydrographic areas, middle Humboldt River basin, north-central Nevada: Methods for estimation and results
No abstract available.
Authors
David L. Berger
Spatial ground-water data base in Carson Valley, Douglas County, Nevada, and Alpine County, California, development and documentation
No abstract available.
Authors
David L. Berger, Rose L. Medina
Hydrogeology and simulated effects of urban development on water resources of Spanish Springs Valley, Washoe County, west-central Nevada
No abstract available.
Authors
D.L. Berger, W.C. Ross, C. E. Thodal, A.R. Robledo
Subsurface flow and water yield from watersheds tributary to Eagle Valley hydrographic area, west-central Nevada
No abstract available.
Authors
D. K. Maurer, D.L. Berger
Subsurface flow to Eagle Valley from Vicee, Ash, and Kings Canyons, Carson City, Nevada, estimated from Darcy's law and the chloride-balance method
No abstract available.
Authors
Douglas K. Maurer, David L. Berger, David E. Prudic
Ground-water conditions and effects of mine dewatering in Desert Valley, Humboldt and Pershing Counties, northwestern Nevada, 1962-91
Desert Valley is a 1,200-square-mile, north- trending, structural basin, about 30 miles northwest of Winnemucca, Nevada. Unconsolidated basin-fill deposits exceeding 7,000 feet in thickness constitute the primary ground-water reservoir. Dewatering operations at an open-pit mine began in the Spring of 1985 in the northeast part of Desert Valley. Ground-water withdrawal for mine dewatering in 1991 w
Authors
D.L. Berger
Lithologic properties of carbonate-rock aquifers at five test wells in the Coyote Spring Valley area, southern Nevada, as determined from geophysical logs
No abstract available.
Authors
D.L. Berger
Ground-water recharge through active sand dunes in northwestern Nevada
Most water-resource investigations in semiarid basins of the Great Basin in western North America conclude that ground-water recharge from direct precipitation on the valley floor is negligible. However, many of these basins contain large areas covered by unvegetated, active sand dunes that may act as conduits for ground-water recharge. The potential for this previously undocumented recharge was i
Authors
D.L. Berger
Principal facts for gravity stations in the Elko, Steptoe Valley, Coyote Spring Valley, and Sheep Range areas, eastern and southern Nevada
Principal facts for 537 gravity stations in the carbonate-rock province of eastern and southern Nevada are tabulated and presented. The gravity data were collected in support of groundwater studies in several valleys. The study areas include the Elko area, northern Steptoe Valley, Coyote Spring Valley, and the western Sheep Range area. The data for each site include values for latitude, longitude,
Authors
D.L. Berger, D.H. Schaefer, E. A. Frick
Ground-water levels in water year 1987 and estimated ground-water pumpage in water years 1986-87, Carson Valley, Douglas County, Nevada
Groundwater levels were measured at 58 wells during water year 1987 and a summary of estimated pumpage is given for water years 1986 and 1987 in Carson Valley, Douglas County, Nevada. The data were collected to provide a record of groundwater changes over the long-term and pumpage estimates that can be incorporated into an existing groundwater model. The estimated total pumpage in water year 1986
Authors
D.L. Berger
Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada
Geophysical logs, drilling operations, pump-test data, and water quality determinations are presented for eight wells in the Coyote Spring Valley area of southeastern Nevada. The wells are in an area where thick units of Paleozoic carbonate rock are overlain by Tertiary semiconsolidated basin-fill deposits and Quaternary alluvial deposits. Data collected by the U.S. Geological Survey were augmente
Authors
D.L. Berger, K. C. Kilroy, D.H. Schaefer
Non-USGS Publications**
Meyer, D.F. and Berger, D.L, 1992, Genoa Folio, Flood and related debris-flow hazards, Genoa quadrangle [Nevada]: Nevada Bureau of Mines and Geology Urban Map Series, Genoa Folio, scale 1:24,000.
Meyer, D.F. and Berger, D.L., 1992, Flood and related debris hazards in the Genoa quadrangle, west-central Nevada: Nevada Bureau of Mines and Geology Open-File Report 92-2.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 26
Water budget estimates for the 14 hydrographic areas in the middle Humboldt River basin, north-central Nevada
Water budgets were developed for the 14 hydrographic areas in the middle Humboldt River Basin of north-central Nevada. The water budgets include estimates of average annual precipitation, runoff, water yield, ground-water recharge and subsurface flow, and evapotranspiration (ET) determined from recently developed or revised methods. Ground-water pumping is not included in the budget estimates. The
Authors
David L. Berger
Water budgets for Pine Valley, Carico Lake Valley, and Upper Reese River Valley hydrographic areas, middle Humboldt River basin, north-central Nevada: Methods for estimation and results
No abstract available.
Authors
David L. Berger
Spatial ground-water data base in Carson Valley, Douglas County, Nevada, and Alpine County, California, development and documentation
No abstract available.
Authors
David L. Berger, Rose L. Medina
Hydrogeology and simulated effects of urban development on water resources of Spanish Springs Valley, Washoe County, west-central Nevada
No abstract available.
Authors
D.L. Berger, W.C. Ross, C. E. Thodal, A.R. Robledo
Subsurface flow and water yield from watersheds tributary to Eagle Valley hydrographic area, west-central Nevada
No abstract available.
Authors
D. K. Maurer, D.L. Berger
Subsurface flow to Eagle Valley from Vicee, Ash, and Kings Canyons, Carson City, Nevada, estimated from Darcy's law and the chloride-balance method
No abstract available.
Authors
Douglas K. Maurer, David L. Berger, David E. Prudic
Ground-water conditions and effects of mine dewatering in Desert Valley, Humboldt and Pershing Counties, northwestern Nevada, 1962-91
Desert Valley is a 1,200-square-mile, north- trending, structural basin, about 30 miles northwest of Winnemucca, Nevada. Unconsolidated basin-fill deposits exceeding 7,000 feet in thickness constitute the primary ground-water reservoir. Dewatering operations at an open-pit mine began in the Spring of 1985 in the northeast part of Desert Valley. Ground-water withdrawal for mine dewatering in 1991 w
Authors
D.L. Berger
Lithologic properties of carbonate-rock aquifers at five test wells in the Coyote Spring Valley area, southern Nevada, as determined from geophysical logs
No abstract available.
Authors
D.L. Berger
Ground-water recharge through active sand dunes in northwestern Nevada
Most water-resource investigations in semiarid basins of the Great Basin in western North America conclude that ground-water recharge from direct precipitation on the valley floor is negligible. However, many of these basins contain large areas covered by unvegetated, active sand dunes that may act as conduits for ground-water recharge. The potential for this previously undocumented recharge was i
Authors
D.L. Berger
Principal facts for gravity stations in the Elko, Steptoe Valley, Coyote Spring Valley, and Sheep Range areas, eastern and southern Nevada
Principal facts for 537 gravity stations in the carbonate-rock province of eastern and southern Nevada are tabulated and presented. The gravity data were collected in support of groundwater studies in several valleys. The study areas include the Elko area, northern Steptoe Valley, Coyote Spring Valley, and the western Sheep Range area. The data for each site include values for latitude, longitude,
Authors
D.L. Berger, D.H. Schaefer, E. A. Frick
Ground-water levels in water year 1987 and estimated ground-water pumpage in water years 1986-87, Carson Valley, Douglas County, Nevada
Groundwater levels were measured at 58 wells during water year 1987 and a summary of estimated pumpage is given for water years 1986 and 1987 in Carson Valley, Douglas County, Nevada. The data were collected to provide a record of groundwater changes over the long-term and pumpage estimates that can be incorporated into an existing groundwater model. The estimated total pumpage in water year 1986
Authors
D.L. Berger
Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada
Geophysical logs, drilling operations, pump-test data, and water quality determinations are presented for eight wells in the Coyote Spring Valley area of southeastern Nevada. The wells are in an area where thick units of Paleozoic carbonate rock are overlain by Tertiary semiconsolidated basin-fill deposits and Quaternary alluvial deposits. Data collected by the U.S. Geological Survey were augmente
Authors
D.L. Berger, K. C. Kilroy, D.H. Schaefer
Non-USGS Publications**
Meyer, D.F. and Berger, D.L, 1992, Genoa Folio, Flood and related debris-flow hazards, Genoa quadrangle [Nevada]: Nevada Bureau of Mines and Geology Urban Map Series, Genoa Folio, scale 1:24,000.
Meyer, D.F. and Berger, D.L., 1992, Flood and related debris hazards in the Genoa quadrangle, west-central Nevada: Nevada Bureau of Mines and Geology Open-File Report 92-2.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.