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Page 5937, results 148401 - 148425

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Publication Extents

Not all publications have extents, not all extents are completely accurate
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
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...
Plant microfossils from the Fort Union Formation
Robert H. Tschudy, Sharon D. Van Loenen
1966, Open-File Report 66-133
As a part of continuing studies to provide palynological data from critical sequences for comparative biostratigraphic studies, the microfossils found in two Paleocene samples have been examined and photographed....
Magnitude and frequency of floods in the United States: Part 10. The Great Basin
E. Butler, J.K. Reid, V.K. Berwick
1966, Water Supply Paper 1684
The probable magnitude of floods of any recurrence interval between 1.1 and 50 years for any stream in the Great Basin can be determined by methods presented in this report.The Great Basin comprises nearly all of Nevada, western Utah, eastern California, and parts of Idaho, Oregon, and Wyoming. The physiography...
Channel and hillslope processes in a semiarid area, New Mexico
Luna Bergere Leopold, William W. Emmett, Robert M. Myrick
1966, Professional Paper 352-G
Ephemeral washes having drainage areas from a few acres to 5 square miles are shown by actual measurement to be accumulating sediment on the streambed. This aggradation is not apparent to the eye but is clearly shown in 7 years of annual remeasurement.A similar aggradation was in progress in the...