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Not all publications have extents, not all extents are completely accurate
Water resources data, Montana, water year 1985; Volume 1. Hudson Bay Basin, Missouri River Basin
R.R. Shields, J. R. Knapton, M. K. White, T.M. Brosten, M.L. Kasman
1986, Water Data Report MT-85-1
The Water Resources Division of the U.S. Geological Survey, in cooperation with State and other Federal agencies, obtain a large amount of data pertaining to the water resources of Montana each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved under-standing...
Reconnaissance of the ground-water, surface-water system in the Zekiah Swamp Run basin, Charles and Prince Georges Counties, Maryland
H. T. Hopkins, G. T. Fisher, L. J. McGreevy
1986, Water-Resources Investigations Report 86-4097
The water table in the alluvium of the Zekiah Swamp Run valley in southern Maryland is above stream level during most of the year and the alluvial aquifer contributes water to the stream. During the summer, however, high evapotranspiration sometimes lowers the water table below the stream level. Water then...
Analyses of flood-flow frequency for selected gaging stations in South Dakota through September 1985
E.B. Hoffman, M.E. Freese, D.R. Winter
1986, Open-File Report 86-496
Analyses of flood-flow frequency were made for 80 active continuous-record gaging stations and 105 discontinued crest-stage partial-record stations in South Dakota with 10 or more years of record. The analyses were developed using the log-Pearson Type III procedure recommended by the U.S. Water Resources Council (Interagency Advisory Committee on Water...
Geohydrology of the Wellington-alluvial aquifer system and evaluation of possible locations of relief wells to decrease saline ground-water discharge to the Smoky Hill and Solomon rivers, central Kansas
Joe B. Gillespie, G.D. Hargadine
1986, Water-Resources Investigations Report 86-4110
Saline water discharges from the alluvial aquifer into the Smoky Hill and Solomon Rivers between New Cambria and Solomon in central Kansas. Chloride concentrations in the Smoky Hill River sometimes exceed 1,000 mg/L during low flow conditions. The source of saline water is the underlying Wellington aquifer, a zone of...
Ground-water data for West Virginia, 1974-84
F.M. Taylor, M.T. Rosier
1986, Open-File Report 86-320
Groundwater investigations began in West Virginia in 1941. As an aid to development and management of the State 's water resources, the U.S. Geological Survey, in cooperation with the West Virginia Geological and Economic Survey, maintains a network of 31 observation wells throughout the State. Some wells are equipped with...
Subsurface injection of liquid waste with emphasis on injection practices in Florida
John J. Hickey, John Vecchioli
1986, Water Supply Paper 2281
Subsurface injection of liquid waste is used as a disposal method in many parts of the country. It is used particularly when other methods for managing liquid waste are either not possible or too costly. Interest in subsurface injection as a waste-disposal method stems partly from recognition that surface disposal...
Water quality of streams and springs, Green River Basin, Wyoming
L. L. DeLong
1986, Water-Resources Investigations Report 82-4008
Data concerning salinity, phosphorus, and trace elements in streams and springs within the Green River Basin in Wyoming are summarized. Relative contributions of salinity are shown through estimates of annual loads and average concentrations at 11 water quality measurements sites for the 1970-77 water years. A hypothetical diversion of 20...
Channel-storage/discharge relations for the Peoria and La Grange dams on the Illinois River in Illinois
George Garklavs, A. R. Klinger, D. M. Mades
1986, Water-Resources Investigations Report 86-4112
The relations between channel storage and discharge at the Peoria and La Grange Dams on the Illinois River are defined. The relations were developed by regressing channel storage against peak discharge at the dams. Peak discharges at the Peoria Dam ranged from 19,700 to 79,500 cu ft/sec, whereas those at...
Shallow ground-water resources in the Grand Strand of South Carolina
G. K. Speiran, W.F. Lichtler
1986, Water-Resources Investigations Report 86-4099
The shallow aquifers that underlie the Grand Strand of South Carolina average approximately 60 to 400 ft thick and have variable productivity with some wells producing little water and others producing several hundred gal/min. These aquifers are separated from the underlying Black Creek aquifer by a 200 ft to 300...
Water resources of the Lower Rio Grande de Arecibo alluvial valley, Puerto Rico
Vicente Quinones-Aponte
1986, Water-Resources Investigations Report 85-4160
An assessment of the surface and groundwater resources of the lower Rio Grande de Arecibo alluvial valley was made between 1981 and 1983. Rio Grande de Arecibo is the major source of water in the valley with a mean-annual discharge of 527 cu ft/sec (382,000 acre-ft/yr). Its lowest mean-daily flow...