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Page 6596, results 164876 - 164900

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Lake Bonneville: Geology and hydrology of the Weber Delta district, including Ogden, Utah
John Henry Frederick Feth, D.A. Barker, L.G. Moore, Randy J. Brown, C.E. Veirs
1966, Professional Paper 518
A cooperative investigation to determine the geology of the Weber Delta district, with emphasis on the occurrence and chemical quality of ground water, was made by the U.S. Geological Survey and the U.S. Bureau of Reclamation with the later assistance of the Utah State Engineer in the final preparation of...
Fresh-water discharge salinity relations in the tidal Delaware River
Walter B. Keighton
1966, Water Supply Paper 1586-G
Sustained flows of fresh water greater than 3,500, 4,400, and 5,300 cubic feet per second into the Delaware River estuary at Trenton, NJ assure low salinity at League Island, Eddystone, and Marcus Hook, respectively. When the discharge at Trenton is less than these critical values, salinity is very sensitive to...
Reservoirs in the United States
R.O.R. Martin, Ronald L. Hanson
1966, Water Supply Paper 1838
This report summarizes the storage capacities and related data of reservoirs and controlled natural lakes for the contermimous United States, Alaska, Hawaii, and the Commonwealth of Puerto Rico. Data are given for all storage facilities having a usable capacity of 5,000 acre-feet or more and completed or under construction as...
Geology of the Arabian Peninsula: Sedimentary geology of Saudi Arabia
R.W. Powers, Leon F. Ramirez, C.D. Redmond, E.L. Elberg Jr.
1966, Professional Paper 560-D
Systematic mapping of the sedimentary geology of Saudi Arabia by Arabian-American Oil Co. (Aramco) began in 1933. By 1959, exploration parties of one type or another had surveyed more than 1,300,000 square kilometers (500,000 square miles) of sedimentary outcrop.The foundation for sedimentary deposition is the Arabian Shield a vast Precambrian...
Organic acids in naturally colored surface waters
William L. Lamar, D.F. Goerlitz
1966, Water Supply Paper 1817-A
Most of the organic matter in naturally colored surface waters consists of a mixture of carboxylic acids or salts of these acids. Many of the acids color the water yellow to brown; however, not all of the acids are colored. These acids range from simple to complex, but predominantly they...
Salinity of the ground water in western Pinal County, Arizona
Lester Ray Kister, W. F. Hardt
1966, Water Supply Paper 1819-E
The chemical quality of the ground water in western Pinal County is nonuniform areally and stratigraphically. The main areas of highly mineralized water are near Casa Grande and near Coolidge. Striking differences have been noted in the quality of water from different depths in the same well. Water from one...
Ground-Water Geology and Hydrology of the Kern River Alluvial-Fan Area, California
R. H. Dale, James J. French, G. V. Gordon
1966, Open-File Report 66-21
The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the 700,000 acre-feet per year flow of...