Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2123
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Publication Extents
Not all publications have extents, not all extents are completely accurateCharles F. Withington, A.J. Froelich
1974, Open-File Report 74-1129
R. H. Wright
1974, Miscellaneous Field Studies Map 573
No abstract available....
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2148
Lawrence J. Mansue, Peter W. Anderson
1974, Water Supply Paper 1798-L
The average annual rate of suspended-sediment discharge of the Stony Brook at Princeton, N.J. (44.5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the Piedmont Lowlands section of the Piedmont physiographic province in west-central New Jersey, range from...
Wayne L. Newell
1974, Open-File Report 74-1079
No abstract available. ...
Gilbert L. Bertoldi
1974, Water-Resources Investigations Report 73-51
Analysis of engineering and hydrologic data from 15 previous soil studies, analysis of particle-size distribution, and analysis of descriptions of soil profiles show that 50 percent of the Sacramento Valley area has soils having permeabilities characterized by infiltration rates of less than 2 feet per day (0.6 meter per day)....
Water Resources Division, U.S. Geological Survey
1974, Water Data Report IL-73-1
Frederick B. Gay, L.G. Toler, Bruce P. Hansen
1974, Hydrologic Atlas 506
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...
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...
G. R. Johnson, C.L. Sainsbury
1974, Geophysical Investigations Map 881
N. Timothy Hall, Andrei M. Sarna-Wojcicki, William R. Dupre
1974, Miscellaneous Field Studies Map 626
This report and map area designed to provide Santa Cruz County with basic data on the location, pattern, recency of movement, potential for future surface rupture, and anticipated earthquake magnitudes and recurrence intervals for several of the faults located there for consideration in the county's land-use planning program and the...
L.C. Dutcher, W. R. Moyle
1974, Water Supply Paper 2007
Fred R. Shawe, Perry B. Wigley
1974, Geologic Quadrangle 1137
James Tazelaar, Wayne L. Newell
1974, Geologic Quadrangle 914
V. A. Frizzell Jr., J.D. Sims, T. H. Nilsen, J. A. Bartow
1974, Miscellaneous Field Studies Map 595
No abstract available....
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.E. Seaburn, D. A. Aronson
1974, Water Supply Paper 2031
An investigation of recharge basins on Long Island was made by the U.S. Geological Survey in cooperation with the New York State Department of Environmental Conservation, Nassau County Department of Public Works, Suffolk County Department of Environmental Control, and Suffolk County Water Authority. The major objectives of the study were...
Karl G. Johnson
1974, Hydrologic Atlas 532
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...
J. E. Cummans
1974, Water-Resources Investigations Report 73-42
Nisqually River flood profiles, covering the reach from near the river mouth to river mile 6.4, were developed in a 2-year field study (1970-72) as part of a continuing program with the State of Washington Department of Ecology. The main channel of the reach will convey without overflow discharges as...
Water Resources Division, U.S. Geological Survey
1974, Open-File Report 74-128
No abstract available....
Water Resources Division, U.S. Geological Survey
1974, Open-File Report 74-17
No abstract available....
H.W. Anderson, D.F. Farrell, W.L. Broussard
1974, Hydrologic Atlas 526
The lower Minnesota River watershed, an area of 2,005 square miles, is fairly flat west of the Minnesota River, but rises to a hilly ridge along the east side of the watershed. Most of the area is covered by ground moraine cut deeply by the Minnesota River and less deeply...