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Page 2392, results 59776 - 59800

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Publication Extents

Not all publications have extents, not all extents are completely accurate
The quality of surface waters in Texas
Jack Rawson
1974, Water-Resources Investigations Report 74-7
The discharge-weighted average concentrations of dissolved solids, chloride, and ,sulfate for many of the principal streams in Texas are less than 500 mg/l (millijgraljls per liter), 250 mg/l, and 250 mg/l, respectively. At 65 of 131 sites on streams that were sampled at least 10 times, the biochemical oxygen demand...
Application of statistical techniques to the estimation of ground-water withdrawals in northwestern Kansas
William M. Kastner
1974, Water-Resources Investigations Report 74-41
This study was made to determine the accuracy of using readily available data with certain statistical techniques to estimate ground-water withdrawals in western Kansas. The data used in the investigation were from a sample of wells chosen from the total inventoried irrigation wells in nine counties in northwestern Kansas; they...
Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York
G.E. Seaburn, D. A. Aronson
1974, Water Supply Paper 2031
An investigation of recharge basins on Long Island was made by the U.S. Geological Survey in cooperation with the New York State Department of Environmental Conservation, Nassau County Department of Public Works, Suffolk County Department of Environmental Control, and Suffolk County Water Authority. The major objectives of the study were...
Seawater intrusion, ground-water pumpage, ground-water yield, and artificial recharge of the Pajaro Valley area, Santa Cruz and Monterey Counties, California
K. S. Muir
1974, Water-Resources Investigations Report 74-9
The Pajaro Valley area, California, covering about 120 square miles (310 km2), extends from the southern part of Santa Cruz County to several miles south of the county line into Monterey County. It borders the Pacific Ocean on the west and the Santa Cruz Mountains on the east. The city...
Water resources data for Michigan, water year 1973; Part 1, Surface water records
Water Resources Division, U.S. Geological Survey
1974, Water Data Report MI-73-1
Surface-water records for the 1973 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Michigan are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water...
Bedrock geologic map of the Greenwood quadrangle, Marquette County, Michigan
William F. Cannon
1974, Geologic Quadrangle 1168
The Marquette Iron Range is presently ( 1973) the second largest iron mining district in the United States. Commercial iron deposits, now mostly concentrating-grade ore, are in the Negaunee Iron-formation, which is part of a thick sequence of metasedimentary rocks of Precambrian X age. These rocks are preserved in the...
Water resources data for Florida, water year 1973; Part 2. Water quality records
Water Resources Division, U.S. Geological Survey
1974, Water Data Report FL-73-2
Water-resources investigations of the U. S. Geological Survey include the collection of water quality data on the chemical and physical characteristics of surface- and ground-water supplies of the Nation. These data for the 1973 water year for the quality of surface waters in Florida are presented in this report. The...
Water resources data for Hawaii and other Pacifica areas, water year 1973
Water Resources Division, U.S. Geological Survey
1974, Water Data Report HI-73-1
Water resources data for the 1973 water year for Hawaii and other Pacific areas including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. The records...
Dissolved-solids discharge to the oceans from the conterminous United States
Donald K. Leifeste
1974, Circular 685
Dissolved-solids data from 54 river basins for 1966-69 were used to compute the amount of dissolved material contributed to the oceans from the conterminous United States. The computations show that about 264,000,000 tons are discharged annually. The Gulf of Mexico receives the largest load, about 183,000,000 tons, of which about...
Sediment transport by streams draining into the Delaware Estuary
Lawrence J. Mansue, Allen B. Commings
1974, Water Supply Paper 1532-H
The quantity of sediment transported by streams draining into the Delaware estuary from Pennsylvania, New Jersey, and Delaware varies areally according to geology, physiography, and land use. Of the estimated total sediment load of 1.6 million tons entering the Delaware estuary annually, about 48 percent is contributed by the Delaware...
Flood characteristics of Oklahoma streams techniques for calculating magnitude and frequency of floods in Oklahoma, with compilations of flood data through 1971
Vernon B. Sauer
1974, Water-Resources Investigations Report 73-52
The 2-, 5-, 10-, 25-, 50-, and 100-year recurrence interval floods are related to basin and climatic parameters for natural streams in Oklahoma by multiple regression techniques through the mathematical model, Qx=aAbScPd,where Qx is peak discharge for recurrence interval x, A is contributing drainage area, S is main channel slope,...
An approach to estimating flood frequency for urban areas in Oklahoma
Vernon B. Sauer
1974, Water-Resources Investigations Report 74-23
Flood-frequency studies for urban areas in several parts of the United States and flood-frequency relations for natural streams of Oklahoma were used to develop a set of flood-frequency equations for urban areas of Oklahoma. Equations arepresented for estimating the 2-, 5-, 10-, 25-, 50-, and 100-year flood-peak discharges for basins...
Flood profiles and inundated areas along the White River, Chelan County, Washington
John Savini, C.F. Schneider, D.E. LaFrance
1974, Water-Resources Investigations Report 74-13
Flood profiles covering the main stem to river mile 11.0 (kilometer 17.7) of the White River in Chelan County, Wash., were developed in a 3-year field study (1970-72) in cooperation with the State of Washington Department of Ecology. Flood-frequency curves based on an average of a regional computation and a...