Water Resources Division, U.S. Geological Survey
1974, Water Data Report IA-73-1
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Page 5539, results 138451 - 138475
Publication Extents
Not all publications have extents, not all extents are completely accurateDonald R. Nichols, Jane M. Buchanan-Banks
1974, Circular 690
Basic earth-science data are necessary for a realistic assessment of seismic hazards and as a basis for limiting corrective land-use controls only to those areas of greatest hazard. For example, the location, character, and amount of likely displacement and activity of surface faulting can be predicted if detailed geologic maps...
Wayne L. Newell
1974, Open-File Report 74-1079
No abstract available. ...
Fred R. Shawe, Perry B. Wigley
1974, Geologic Quadrangle 1137
Henry L. Berryhill
1974, Circular 694
At the end of 1972, offshore petroleum exploration was in progress on the submerged continental margins of 80 countries. Some 780 oil and gas fields had been discovered. Estimated worldwide volume of oil discovered offshore as of January 1, 1973, is 172.8 billion barrels of oil, or about 26 percent...
Robert L. Detterman
1974, Miscellaneous Field Studies Map 584
A fence diagram of the Sadlerochit Formation, the major reservoir rock in the Prudhoe Bay oil field, is presented for about 20,000 square miles of northeastern Alaska. Thirty reference points were used in constructing the diagram, 27 are outcrop sections measured in detail between 1969 and 1972, and 4 are...
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2142
Dean O. Gregg, Everett Alfred Zimmerman
1974, Water Supply Paper 2029-D
Water from a brackish-water zone (1,050-1,350 ft) has concentrations as high as 2,150 milligrams per liter chloride, and concentrations are suspected to be higher than 3,000 milligrams per liter chloride. This brackish water has been identified as the source of the water that contaminates the upper and lower fresh-water-bearing zones...
R. W. Page
1974, Water-Resources Investigations Report 73-45
The Sacramento Valley, which forms most of the northern one-third of the Central Valley, is a broad structural trough. The study area comprises the valley floor and some of the foothills of the Sierra Nevada and the Coast Ranges, a total area of about 6,000 square miles.Beneath most places in...
Adel A. R. Zohdy
1974, Bulletin 1313-D
Arthur E. Nelson
1974, Bulletin 1395-E
Edwin D. Gutentag, Lloyd E. Stullken
1974, Hydrologic Atlas 515
W. C. Swadley
1974, Geologic Quadrangle 1154
George Clarke Simmons
1974, Geologic Quadrangle 1130
Water Resources Division, U.S. Geological Survey
1974, Open-File Report 74-206
J. Hiram Smith
1974, Geologic Quadrangle 1197
B. Carter Hearn, Jr.
1974, Open-File Report 74-23
C.S. Wotorson, John C. Behrendt
1974, IMAP 777-B
R. A. Wobus, R.C. Epis
1974, Open-File Report 74-95
E. R. Hampton, G. A. Clark, M. H. McNutt
1974, IMAP 855-C
No abstract available....
G. H. Davis, Leonard A. Wood
1974, Circular 703
Water is used in producing energy for mining and reclamation of mined lands, onsite processing, transportation, refining, and conversion of fuels to other forms of energy. In the East, South, Midwest, and along the seacoasts, most water problems are related to pollution rather than to water supply. West of about...
James Tazelaar, Wayne L. Newell
1974, Geologic Quadrangle 914
Robert Denny Trace
1974, Geologic Quadrangle 1201
L.G. Davis
1974, Circular 710
This manual provides methods for estimating the magnitude and frequency of floods on unregulated and unurbanized streams in Indiana that drain at least 15 square miles (38.8 square kilometres). The methods provide the design engineer with a means of estimating flood frequencies without having to analyze the records at individual...
G. R. Johnson, C.L. Sainsbury
1974, Geophysical Investigations Map 881