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Page 6577, results 164401 - 164425

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Publication Extents

Not all publications have extents, not all extents are completely accurate
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...
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...
Ground-water resources of Sheridan County, Wyoming
Marlin E. Lowry, T. Ray Cummings
1966, Water Supply Paper 1807
Sheridan County is in the north-central part of Wyoming and is an area of about 2,500 square miles. The western part of the county is in the Bighorn Mountains, and the eastern part is in the Powder River structural basin. Principal streams are the Powder and Tongue Rivers, which are...
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...
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...
River meanders - Theory of minimum variance
Walter Basil Langbein, Luna Bergere Leopold
1966, Professional Paper 422-H
Meanders are the result of erosion-deposition processes tending toward the most stable form in which the variability of certain essential properties is minimized. This minimization involves the adjustment of the planimetric geometry and the hydraulic factors of depth, velocity, and local slope.The planimetric geometry of a meander is that of...
Geological Survey research 1966, Chapter B
Water Resources Division, U.S. Geological Survey
1966, Professional Paper 550-B
This collection of 43 short papers is the first published chapter of 'Geological Survey Research 1966.' The papers report on scientific and economic results of current work by members of the Conservation, Geologic, Topographic, and Water Resources Divisions of the U.S. Geological Survey. Chapter A, to be published later in...
Geological Survey Research 1966, Chapter A
Water Resources Division, U.S. Geological Survey
1966, Professional Paper 550-A
'Geological Survey Research 1966' is the seventh annual review of the econamic and scientific work of the U.S. Geological Survey. As in previous years the purpose of the volume is to make available promptly to the public the highlights of Survey investigations. This year the volume consists of 4 chapters...