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Page 5581, results 139501 - 139525

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Not all publications have extents, not all extents are completely accurate
Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota
Thomas C. Winter
1973, Water Supply Paper 2029-A
Stratified fluvial sediments occur within the glacial drift at many places in the Mesabi Iron Range area. These sediments, which are important aquifers, occur extensively between the three main till units. The thickest and most extensive aquifer consists of glaciofluvial sediments that lie between the surficial till and the middle...
Fluvial sediment characteristics of the Kansas River at Wamego, Kansas, 1957-70
C.D. Albert
1973, Open-File Report 73-2
Fluvial-sediment samples have been collected from the Kansas River at Wamego from 1957-70 by the U.S. Geological Survey in cooperation with the Kansas Water Resources Board. During this period. the stream-runoff pattern of the basin has been altered by constructions of Tuttle Creek and Milford Reservoirs. An analysis of data shows...
Fluvial sediment in Double Creek subwatershed No. 5, Washington County, Oklahoma
Gene A. Bednar, Thomas E. Waldrep
1973, Open-File Report 73-22
Double Creek subwatershed No. 5 in Washington County, Oklahoma, is one of six detention structures within the Double Creek watershed and includes 1,530 acres (2.39 square miles). The subwatershed receives runoff from approximately 5 percent of the total area of the watershed. Most precipitation falling on subwatershed No. 5 does not...
Cost analysis of ground-water supplies in the North Atlantic region, 1970
Dagfin John Cederstrom
1973, Water Supply Paper 2034
The cost of municipal and industrial ground water (or, more specifically, large supplies of ground water) at the wellhead in the North Atlantic Region in 1970 generally ranged from 1.5 to 5 cents per thousand gallons. Water from crystalline rocks and shale is relatively expensive. Water from sandstone is less...
Availability of water from limestone and dolomite aquifers in southwest Ohio and the relation of water quality to the regional flow system
Stanley Eugene Norris, Richard E. Fidler
1973, Water-Resources Investigations Report 73-17
The largest ground-water supplies from the 150 to 450-foot thick carbonate-rock aquifer in southwest Ohio are available in a 2,800 squaremile area on the crest and eastern flank of the Cincinnati arch. Well production in the high-yield area is mainly from the Newburg zone, a permeable stratum in the lower...