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16498 results.

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Page 601, results 15001 - 15025

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Not all publications have extents, not all extents are completely accurate
Water resources of Wisconsin — Trempealeau-Black River basin
H. L. Young, Ronald G. Borman
1973, Hydrologic Atlas 474
The purpose of this report is to describe the physical environment, availability, characteristics, distribution, movement, and quality of water in the lower Wisconsin River basin. In addition, water use and water problems are summarized to aid in water management within the basin. Detailed water studies will be necessary as the...
Preliminary photointerpretation map of landslide and other surficial deposits of the Concord 15-minute quadrangle and the Oakland West, Richmond, and part of the San Quentin 7 1/2-minute quadrangles, Contra Costa and Alameda Counties, California
T. H. Nilsen
1973, Miscellaneous Field Studies Map 493
This map presents preliminary information about one aspect of the physical environment necessary to sound land-use planning- the nature and distribution of surficial deposits.  Because surficial deposits are common and well developed in much of the bay region, it is useful to know how and why they have formed, as...
Water resources of Wisconsin, Pecatonica-Sugar River basin
S. M. Hindall, Earl L. Skinner
1973, Hydrologic Atlas 453
The purpose of this report is to describe the physical environment, availability, characteristics, distribution, movement, and quailty of water in the Pecatonica-Sugar River basin.  In addition, water use and water problems are summarized to give an understanding of man's management of water within the basin....
Floods of 1971 and 1972 on Glover Creek and Little River in southeastern Oklahoma
Wilbert O. Thomas, Robert K. Corley
1973, Water-Resources Investigations Report 73-5
Heavy rains of December 9-10, 1971, and Oct. 30-31, 1972, caused outstanding floods on Glover Creek and Little River in McCurtain County in southeastern Oklahoma. This report presents hydrologic data that document the extent of flooding, flood profiles, and frequency of flooding on reaches of both streams. The data presented...
Reconnaissance of the water resources of Beaver County, Oklahoma
Robert B. Morton, R. L. Goemaat
1973, Hydrologic Atlas 450
Ground water is the major source of water supply in Beaver County. Because of the rapidly increasing demand for the limited supply of water for irrigation, additional geologic and hydrologic data are needed for management of ground-water resources. This report presents general information on the availability of ground water, on...
Electric-analog simulation network of unconsolidated aquifers in the upper Wabash River basin, Indiana
James E. Heisel
1973, Water-Resources Investigations Report 73-29
The ground-water budget of the unconsolidated deposits in the upper Wabash River basin was modeled. An electrical-simulation network was used to determine an integrated storage coefficient of 0.003 for the basin. Two practical problems were investigated: a municipal pumping problem and the change in flow regime due to the addition...
Ground-water hydrology of northern Napa Valley, California
Robert E. Faye
1973, Water-Resources Investigations Report 73-13
The alluvium of northern Napa Valley is the principal aquifer of the area and is capable of yielding as much as 3,000 gallons per minute to wells. Generally the larger-yielding wells are along the Napa River where the alluvium is thickest and most permeable. Recharge to the alluvium is chiefly...
Flood of June 9-10, 1972, at Rapid City, South Dakota
Owen J. Larimer
1973, Hydrologic Atlas 511
Rapid City, the second largest city in South Dakota, is located at the eastern edge of the Black Hills about 9 miles downstream from Pactola Dam.  It is bisected laterally by Rapid Creek, and longitudinally by the eastern flank of the Black Hills.  Canyon Lake, a samll recreation reservior having...