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Page 5679, results 141951 - 141975

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Quality of surface water in the Bear River basin, Utah, Wyoming, and Idaho
K.M. Waddell, Don Price
1972, Hydrologic Atlas 417
The United States Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Water Rights, began a reconnaissance in 1967 to obtain essential water-quality information for the Bear River basin. The reconnaissance was directed toward defining the chemical quality of the basin’s surface waters, including suitability for...
Water resources of the Minnesota River-Hawk Creek watershed, southwestern Minnesota
Wayne A. Van Voast, W.L. Broussard, D.E. Wheat
1972, Hydrologic Atlas 391
The Minnesota River – Hawk Creek watershed is located in southwestern Minnesota. The watershed has an area of 1,479 square miles and is drained along its southwestern edge by the Minnesota River (Minnesota Division of Waters, 1959). The major watercourse within the watershed is Hawk Creek, having a drainage area...
Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas
Marion S. Hines, Raymond O. Plebuch, A. G. Lamonds
1972, Hydrologic Atlas 377
Water is available in Clay, Greene, Craighead, and Poinsett Counties from ground-water and surface-water sources. However, ground water is more accessible in many places than surface water. Ground water is available from the alluvium, which covers all the area except Crowleys Ridge, and is also available from other formations below...
Fluvial sediment in Salem Fork watershed, West Virginia
R.F. Flint
1972, Water Supply Paper 1798-K
Suspended sediment discharged from the 8.32-square-mile Salem Fork study area in Harrison County, W. Va., averaged 3,500 tons per year during the first 4-year period of investigation and 1,770 tons per year during the second 4-year period. The difference as attributed to increased flow control, effected by the completion of...
Fluvial sediment in Hocking River subwatershed 1 (North Branch Hunters Run), Ohio
R.F. Flint
1972, Water Supply Paper 1798-I
From May 1956 to May 1962, Hocking River subwatershed 1 of Upper Hocking River Pilot Watershed had an average annual sediment yield from its contributing area of 0.94 square mile of 1,195 tons per square mile. Annual suspended-sediment yield at the outlet, expressed in tons per acre-foot of outflow, decreased...
Sand transport by the Eel River and its effect on nearby beaches
John R. Ritter
1972, Open-File Report 73-236
The Eel River basin has one of the largest sediment yields per unit area in the world. Sand composes about 25 percent of the total sediment transported by the river into its estuary. The annual sand load averages about 4,600,000 tons, equivalent to a deposition of about 2,100 acre-feet of...