W.L. Broussard, H.W. Anderson, D.F. Farrell
1973, Hydrologic Atlas 466
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Page 598, results 14926 - 14950
Publication Extents
Not all publications have extents, not all extents are completely accurateCharles A. Appel
1973, Open-File Report 73-9
Charles K. Bayne
1973, Hydrologic Atlas 462
Roman T. Mycyk, R. Stephen Grant
1973, Hydrologic Atlas 497
D. B. Sapik, R. L. Goemaat
1973, Hydrologic Atlas 373
No abstract available....
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...
J. H. Robison
1973, Hydrologic Atlas 480
J. W. Warner, J. A. Moreland
1973, Open-File Report 73-358
This is a study of the feasibility of recharging, in the Waterman Canyon-East Twin Creek area, imported water from northern California by way of the State Water Project beginning in 1972. The feasibility of recharging 30,000 acre-feet of water a year in the Waterman Canyon-East Twin Creek area will depend...
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...
Glenn C. Prescott
1973, Hydrologic Atlas 486
No abstract available....
J. H. Robison
1973, Open-File Report 73-241
Hydrology of a 20-square-mile area of dunes along the central Oregon coast was studied. The area is underlain by 80 to 150 feet of Quaternary dune and marine sand which overlies Tertiary marine clay and shale. Ground water for industrial and municipal use is being withdrawn at a rate of...
Richard A. Brackley, William B. Fleck, Walter Richard Meyer
1973, Hydrologic Atlas 484
Leland Vernon Page, L. C. Shaw
1973, Hydrologic Atlas 530
No abstract available....
R. W. Page
1973, Hydrologic Atlas 489
Thomas M. Ushijima, Charles J. Ewart
1973, Hydrologic Atlas 473
No abstract available....
J. F. Ficke, J.B. Weeks, F.A. Welder
1973, Open-File Report 73-71
Harold A. Whitcomb
1973, Hydrologic Atlas 441
B. K. Holmstrom, W.A. Gebert, Ronald G. Borman
1973, Open-File Report 74-1049
The purpose of this study was to determine the hydrologic characteristics of Alder Creek, Iron County, Wisconsin, which are needed by water-resource planners to evaluate a reservoir site proposed by the Whitecap Mountain Corporation on Alder Creek. The hydrologic characteristics estimated were the mean flows, low flows, flood peaks, suspended-sediment...
Glenn C. Prescott
1973, Hydrologic Atlas 485
No abstract available....
E.J. Kennedy
1973, Open-File Report 73-142
A flood insurance study, made for the Federal Insurance Administration (FIA) of the Department of Housing and Urban Development (HUD) is an analysis of flood inundation frequency for all flood plains within the corporate limits of the community being studied. The study is an application of surveying, hydrology, and hydraulics...
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...
C.F. Keech, J.E. Moore, P. A. Emery
1973, Open-File Report 73-139
A "Level B" study is being made of the Platte River basin in Nebraska. The basin (approximately 40,800 square miles) extends the full length of the State, a distance of nearly 470 miles. The study is a Federal and State interagency effort to formulate a comprehensive plan for the conservation,...
B.L. Jones, C.J. Ewart
1973, Open-File Report 73-134
The first 2 years of intensive data collection in Moanalua Valley have resulted in some observations concerning the rainfall-runoff and rainfall-sedimentation characteristics of the basin.This initial study period has been concerned primarily with establishing a reliable hydrologic data-collection network. However, enough data have been collected to determine that rainfall within...
Michael H. Frimpter
1973, Open-File Report 73-76
R. W. Page, Gary O. Balding
1973, Water-Resources Investigations Report 73-6
The Modesto-Merced area includes about 1,800 square miles on the northeast side of the San Joaquin Valley. The physiographic units in the area are (1) Sierra Nevada, (2) dissected uplands, (3) low alluvial plains and fans, (4) river flood plains and channels, and (5) overflow lands.Geologic units consist of consolidated...