R. K. Hose
1974, IMAP 831
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Page 5539, results 138451 - 138475
Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1974, IMAP 875-A
N. J. King
1974, IMAP 848-E
No abstract available....
John R. Williams, Gary D. Tasker
1974, Hydrologic Atlas 507
Marvin L. Schroeder
1974, Geologic Quadrangle 1160
W.L. Yonts, G. L. Giese
1974, Water-Resources Investigations Report 74-11
Three levels of thermal loading of Hyco Lake by heat from two steam-electric generators have resulted in higher temperatures and increased evaporation in the 3,750-acre (1,518 square hectometer) lake. During the winter, local temperature increases of 34°F (19°C) were sometimes observed at the surface as heated water spread out on...
Henry W. Roehler
1974, Geologic Quadrangle 1200
Vernon Emanuel Swanson
1974, Open-File Report 74-197
A geologic-geochemical evaluation conducted October 5-24, 1968, both in the field area and in the laboratories has shown the Upper Cretaceous oil shale in the El Lajjun area of central Jordan to be one of Jordan's major natural mineral resources. Continued but slightly modified investigations are strongly recommended to determine...
W. J. Hail Jr.
1974, Miscellaneous Field Studies Map 619
J. Hiram Smith
1974, Geologic Quadrangle 1197
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. 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...
Frederick B. Gay, L.G. Toler, Bruce P. Hansen
1974, Hydrologic Atlas 506
Water Resources Division, U.S. Geological Survey
1974, Open-File Report 74-208
G. R. Johnson, C.L. Sainsbury
1974, Geophysical Investigations Map 881
B. Carter Hearn, Jr.
1974, Open-File Report 74-23
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...
Robert Wayne Schnabel
1974, Geologic Quadrangle 1170
George Clarke Simmons
1974, Geologic Quadrangle 1130
Adel A. R. Zohdy
1974, Bulletin 1313-D
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...
R.L. Melvin, F.P. Haeni
1974, Open-File Report 74-320
Water Resources Division, U.S. Geological Survey
1974, Open-File Report 74-8
Herbert E. Skibitzke
1974, Open-File Report 77-643
Remote sensing data were taken along a line surveyed for the building of the Alyeska Pipeline, Alaska, in the winter of 1973-74. The portion considered in this report is the area from the Yukon River south to Isabel Pass in the Alaska Range. The occurrences of aufeis gave the appearance...
W. C. Swadley
1974, Geologic Quadrangle 1154