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Stage-discharge relations for Black Warrior River at Warrior Dam near Eutaw, Alabama; updated 1985
G. H. Nelson, C. O. Ming
1986, Open-File Report 85-698
The construction of Warrior Dam, completed in 1962, has resulted in changes to the stage-discharge relations in the vicinity. The scarcity of current-meter measurements, coupled with backwater conditions, make definition of a single stage-discharge relation impossible without considerable error. However, as a useful alternative, limit curves were developed in 1983...
Geological and geochemical data for seamounts and associated ferromanganese crusts in the Ratak Chain, Marshall Islands
W. C. Schwab, J.R. Hein, A. S. Davis, L.A. Morgenson, C.L. Daniel, J.A. Haggerty
1986, Open-File Report 86-338
In 1984, the U.S. Geological Survey (USGS) conducted a reconnaissance cruise L9-84-CP aboard the R/V S.P. LEE along the northern Ratak Ridge, Marshall Islands (Fig. 1). Preliminary geochemical results from the cruise show that ferromanganese crusts (Mn crusts) on the submarine slopes of seamounts, and islands may have potential for...
Preliminary report on geophysical well-logging activity on the Salton Sea Scientific Drilling Project, Imperial Valley, California
Frederick L. Paillet, R. H. Morin, H.E. Hodges
1986, Open-File Report 86-544
The Salton Sea Scientific Drilling Project has culminated in a 10,564-ft deep test well, State 2-14 well, in the Imperial Valley of southern California. A comprehensive scientific program of drilling, coring, and downhole measurements, which was conducted for about 5 months, has obtained much scientific information concerning the physical and...
Ground-water and surface-water-level data at Rindge Tract on the Stockton Deep Water Ship Channel, San Joaquin County, California, 1983-84
Michael J. Pierce, Karen L. Johnson
1986, Open-File Report 85-573
The Sacramento-San Joaquin Delta is formed at the confluence of the two major rivers that drain the Central Valley of California. The Sacramento and San Joaquin Rivers and many interconnecting sloughs meandered back and forth across the tidelands, frequently overflowing their banks. Approximately 1 ,100 miles of levees were constructed...