Charles Sherwood Robinson, Lawrence Allen Warner, Ernest Eugene Wahlstrom
1974, Professional Paper 831-B
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Publication Extents
Not all publications have extents, not all extents are completely accurateJohn C. Behrendt, C.S. Wotorson
1974, IMAP 771-B
George Plafker
1974, Open-File Report 74-82
No abstract available....
D. H. Eargle, K. A. Dickinson
1974, Open-File Report 74-43
Water Resources Division, U.S. Geological Survey
1974, Water Data Report MI-73-1
Surface-water records for the 1973 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Michigan are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water...
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...
Edward Huntington Cobb
1974, Mineral Investigations Resource Map 61
No abstract available....
Nancy A. Wright, Paul L. Williams, editor(s)
1974, Circular 705
Although the existence of mineral deposits in Antarctica is highly probable, the chances of finding them are quite small. Minerals have been found there in great variety but only as occurrences. Manganese nodules, water (as ice), geothermal energy, coal, petroleum, and natural gas are potential resources that could perhaps be...
Edwin D. Gutentag, Lloyd E. Stullken
1974, Hydrologic Atlas 515
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...
Donald B. Hoover
1974, Open-File Report 74-1050
No abstract available....
Robert L. Christiansen
1974, Geologic Quadrangle 1191
Robert Wayne Schnabel
1974, Geologic Quadrangle 1170
Robert L. Christiansen, H. Richard Blank
1974, Geologic Quadrangle 1190
R. A. Wobus, R.C. Epis
1974, Open-File Report 74-95
H. Roberta Dixon
1974, Geologic Quadrangle 1165
Melville Rhodes Mudge, Robert L. Earhart, Kenneth C. Watts Jr., Ernest T. Tuchek, William L. Rice
1974, Bulletin 1385-B
No abstract available....
George Clarke Simmons
1974, Geologic Quadrangle 1130
John S. Pomeroy
1974, Open-File Report 74-116
James George Evans
1974, Geologic Quadrangle 1116
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...
Henry W. Roehler
1974, Geologic Quadrangle 1166
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...
R.L. Melvin, F.P. Haeni
1974, Open-File Report 74-326
B. Carter Hearn, Jr.
1974, Open-File Report 74-23