Publications
This list of Water Resources Mission Area publications includes both official USGS publications and journal articles authored by our scientists. A searchable database of all USGS publications can be accessed at the USGS Publications Warehouse.
Filter Total Items: 18418
Geology and ground water of the Savannah River Plant and vicinity, South Carolina
The area described in this report covers approximately 2,600 square miles in west-central South Carolina and includes the site of the Savannah River Plant, a major production facility of the U.S. Atomic Energy Commission. The climate, surface drainage, and land forms of the study area are typical of the southern part of the Atlantic Coastal Plain. Precipitation is normally abundant and fairly even
Authors
George E. Siple
Ground-water reconnaissance in the Burnt River Valley area, Oregon
No abstract available.
Authors
Don Price
Ground water in the Eola-Amity Hills area, northern Willamette Valley, Oregon
The Eola-Amity Hills area ,comprises about 230 square miles on the west side of the Willamette Valley between Salem and McMinnville, Oreg. The area is largely rural, and agriculture is the principal occupation.
Rocks ranging in age from Eocene to Recent underlie the area. The oldest rocks are a sequence more than 5,000 feet thick of marine-deposited shale and siltstone strata, with thin interb
Authors
Don Price
Geology and water resources in the French Prairie area, northern Willamette Valley, Oregon
No abstract available.
Authors
Don Price
Geohydrology of the Souris River Valley in the vicinity of Minot, North Dakota
The Minot area is in the north-central part of North Dakota and includes part of the Souris River valley. The region is covered by glacial drift of late Wisconsin age except in small areas where the Fort Union Formation of Tertiary age crops out. Thickness of the drift is controlled by the topography of the bedrock. In places the drift is more than 450 feet thick, but it averages about 100 feet th
Authors
Wayne A. Pettyjohn
Causes of fluctuations in the rate of discharge of Clear Lake Springs, Millard County, Utah
The Clear Lake Springs in southeastern Millard County are the source of water for the maintenance of the Clear Lakes Migratory Waterfowl Refuge. Seasonal declines in the rate of discharge were noted during 1959-60.Fluctuations in the flow of Clear Lake Springs are caused both by natural variations in the quantity of recharge and by variations in the quantity of water pumped from an increasing numb
Authors
R. W. Mower
Correlation and analysis of water-temperature data for Oregon streams
No abstract available.
Authors
A.M. Moore
Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60
The Hydrologic Laboratory was established in 1948 to serve as the central testing laboratory for the Water Resources Division of the U.S. Geological Survey. Since then, thousands of samples of rock and soil materials have been analyzed in the laboratory. Analytical data on samples from 42 States and for the period 1948-60 are summarized in this report.
The data are presented in a form that all
Authors
D. A. Morris, A.I. Johnson
Chemical quality of surface water in the Allegheny River basin, Pennsylvania and New York
The Allegheny River is the principal source of water to many industries and to communities in the upper Ohio River Valley. The river and its many tributaries pass through 19 counties in northwestern and western Pennsylvania. The population in these counties exceeds 3 million. A major user of the Allegheny River is the city of Pittsburgh, which has a population greater than The Allegheny River is a
Authors
Edward F. McCarren
Reconnaissance of the chemical quality of surface waters of the Neches River basin, Texas
The kinds and quantities of minerals dissolved in the surface water of the Neches River basin result from such environmental factors as geology, streamflow patterns and characteristics, and industrial influences. As a result of high rainfall in the basin, much of the readily soluble material has been leached from the surface rocks and soils. Consequently, the water in the streams is usually low in
Authors
Leon S. Hughes, Donald K. Leifeste
Artificial recharge through a well tapping basalt aquifers at the Dalles, Oregon
No abstract available.
Authors
B. L. Foxworthy, Charles T. Bryant
Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah
The upper Sevier River basin is in south-central Utah and includes an area of about 2,400 .square miles of high plateaus and valleys. It comprises the entire Sevier River drainage basin above Kingston, including the East Fork Sevier River and its tributaries. The basin was investigated to determine general ground-water conditions, the interrelation of ground water and surface water, the effects of
Authors
Carl H. Carpenter, Gerald B. Robinson, Louis Jay Bjorklund