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Page 2139, results 53451 - 53475

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Not all publications have extents, not all extents are completely accurate
Map showing selected surface-water data for the Alton-Kolob coal-fields area, Utah
Don Price
1982, IMAP 1235-D
This is one of a series of maps that describe the geology and related natural resources of the Alton-Kolob coal-fields area, Utah. Streamflow records used to compile the map and the following table were collected by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division...
Dissolved-solids concentrations of ground water in the Sacramento Valley, California
Ronald P. Fogelman
1982, Hydrologic Atlas 645
The general quality of the ground water in the Sacramento Valley , Calif., in terms of dissolved-solids concentration is considered good for irrigation, domestic, and most other uses. This map shows the distribution of dissolved-solids concentrations and is based on about 1,330 chemical analyses collected from about 900 wells between...
Geohydrology of the Standing Rock Indian Reservation, North and South Dakota
Lewis W. Howells
1982, Hydrologic Atlas 644
Effective improvement of economic and social conditions of Indians living on the Standing Rock Indian Reservation has been hampered by lack of adequate and reliable information about the quantity and quality of water supplies available for development.  Compounding the problem is the recent filling of Oahe Reservoir (now Lake Oahe),...
Water Resources Data Hawaii, other Pacific Areas, water year 1981: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau Islands and American Samoa
Water Resources Division, U.S. Geological Survey
1982, Water Data Report HI-81-2
Volume 2 of water resources data for the 1981 water year for other Pacific areas consist of records of stage, discharge, and water quality of streams; stage of a reservoir; and water levels in wells and springs. This report contains discharge records for 41 gaging stations; stage only record for...
Techniques for estimating magnitude and frequency of floods in South Carolina
Benjamin H. Whetstone
1982, Water-Resources Investigations Report 82-1
Methods are provided for estimating flood magnitudes at recurrence intervals of 2, 5, 10, 25, 50, and 100 years, for unregulated rural streams in South Carolina with drainage areas greater than 1.0 square mile. Multiple regression analyses were used to define the relation between flood discharge and basin and climatic...
Water resources data for Missouri, water year 1981
Water Resources Division, U.S. Geological Survey
1982, Water Data Report MO-81-1
Water resources data for the 1981 water year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 124 gaging stations; stage and contents at 7 lakes and reservoirs; water quality at 33 gaging stations (including 1 lake); 11...
Water resources data for Arizona, water year 1980
Water Resources Division, U.S. Geological Survey
1982, Water Data Report AZ-80-1
Water resources data for the 1980 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; water levels of observation wells; and quality of ground water. This report contains discharge records for 240 gaging stations, annual...
Effects of a floodwater-retarding structure on the hydrology and ecology of Trout Creek in southwestern Wisconsin
Steve Baima, David J. Graczyk, Stephen J. Field, Dennis A. Wentz, William L. Hilsenhoff, Eddie L. Avery, O. M. Brynildson
Dennis A. Wentz, David J. Graczyk, editor(s)
1982, Water-Resources Investigations Report 82-23
The primary effects of a floodwater-retarding structure (FRS) on the streamflow of Trout Creek, Wisconsin, are attenuation of flood peaks and extension of the time base of flood hydrographs. Reduction of flood peaks ranged from 58 to 91 percent during the study period from 1975 to 1979. There is an inverse...
Land subsidence in the San Joaquin Valley, California, as of 1980
R. L. Ireland, J. F. Poland, F. S. Riley
1982, Open-File Report 82-370
Land subsidence due to ground-water overdraft in the San Joaquin Valley began in the mid-1920 's and continued at alarming rates until surface was imported through major canals and aqueducts in the 1950 's and late 1960's. In areas where surface water replaced withdrawal of ground-water, water levels in the...