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Page 2528, results 63176 - 63200

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Fluvial sediment in the little Arkansas River basin, Kansas
C.D. Albert, G.J. Stramel
1966, Water Supply Paper 1798-B
Characteristics and transport of sediment in the Little Arkansas River basin in south-central Kansas were studied to determine if the water from the river could be used as a supplemental source for municipal supply or would provide adequate recharge to aquifers that are sources of municipal and agricultural water supplies....
Annual runoff in the conterminous United States
Mark W. Busby
1966, Hydrologic Atlas 212
Runoff is that part of precipitation that appears as a flow of water in surface streams. As a source of water for modern society, it constitutes one of our basic renewable resources. This map of average annual runoff portrays the latest information on the geographic distribution of the average runoff...
Temperature of surface waters in the conterminous United States
James F. Blakey
1966, Hydrologic Atlas 235
Temperature is probably the most important, but least discussed, parameter in determining water quality. The purpose of this report is to present the average or most probable temperatures of surface waters in the conterminous United States and to cite factors that affect and are affected by water temperature. Temperature is...
Evaporation study in a humid region, Lake Michie, North Carolina
J.F. Turner Jr.
1966, Professional Paper 272-G
The mass-transfer and water-budget techniques of calibrating a reservoir for evaporation were evaluated through a study of Lake Michie, N.C. The techniques appear adequate for estimation of lake evaporation and net seepage in humid regions where lake storage is affected by streamflow and ground-water seepage, under conditions no more adverse...
Summer base-flow recession curves for Iowa streams
C.W. Saboe
1966, Open-File Report 66-120
Base-flow recession. curves for the summer months (June through September) were developed in this study for gaging stations on interior Iowa streams having five or more years of record. The tabulated data enables the user, starting with a known base flow at a gage, to estimate base flows for up...
Arizona Water
John William Harshbarger, D.D. Lewis, H.E. Skibitzke, W. L. Heckler, L. R. Kister, H. L. Revised by Baldwin
1966, Water Supply Paper 1648
Water resources of the Pomme de Terre River Watershed, West-central Minnesota
R. D. Cotter, L. E. Bidwell
1966, Hydrologic Atlas 220
The watershed is underlain by water-bearing glacial drift, cretaceous rocks, and Precambrian crystalline rocks.  It is an elongate basin 92 miles long and has a drainage area of 977 square miles.  The Pomme de Terre River flows within an outwash valley discharging into the Minnesota River at Marsh Lake....
Induced recharge of an artesian glacial-drift aquifer at Kalamazoo, Michigan
J.E. Reed, Morris Deutsch, S.W. Wiitala
1966, Water Supply Paper 1594-D
As part of a program for managing its ground-water supply, the city of Kalamazoo has constructed induced-recharge facilities at the sites of several of its well fields. To determine the benefits of induced recharge in a water-management program, the U.S. Geological Survey, in cooperation with the city, conducted a series...