Water Resources Division, U.S. Geological Survey
1972, Bulletin 1269
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Publication Extents
Not all publications have extents, not all extents are completely accurateF. C. W. Dodge
1972, Bulletin 1314-F
Roman T. Mycyk, R. Stephen Grant
1972, Hydrologic Atlas 464
Otto Moosburner
1972, Hydrologic Atlas 215
No abstract available....
Roman T. Mycyk, Marvin D. Duerk
1972, Hydrologic Atlas 459
Aelred D. Geis, F. Graham Cooch
1972, Special Scientific Report - Wildlife 151
Charles Richard Murray, E. Bodette Reeves
1972, Circular 676
Estimates of water use in the United States in 1970 indicate that an average of about 370 bgd (billion gallons per day)about 1,800 gallons per capita per day--was withdrawn for the four principal off-channel uses which are (1) public-supply (for domestic, commercial, and industrial uses), (2) rural (domestic and livestock),...
E. F. Hubbard, William G. Stamper
1972, Water Supply Paper 1873-E
This report presents the results of a fluorescent-dye-tracing study to determine the concentrations of a pollutant that would be present in the Northeast Cape Fear Estuary at various rates of continuous waste injection and freshwater inflow. Rhodamine WT dye was introduced into the estuary at a constant rate over a...
R. W. Bayley
1972, IMAP 712
Water Resources Division, U.S. Geological Survey
1972, Water Data Report AR-71-1
Kenneth F. Williams, Lloyd A. Reed
1972, Water Supply Paper 1532-F
The Susquehanna River presently transports about 3.0 million tons of sediment annually (110 tons per square mile). Only about 1.8 million tons of sediment enters the head of Chesapeake Bay annually because some sediment is trapped behind the power dams on the lower Susquehanna. Measured annual sediment yields from subbasins...
D.A. Webster
1972, Miscellaneous Field Studies Map 453
No abstract available....
J.D. Stoner
1972, Water Supply Paper 1873-F
During a study of the effects of waste-water input on the stratified Duwamish River estuary, intensive water-velocity and salinity measurements were made in both the lower salt wedge and the upper fresher water layer for tidal-cycle periods. The net movement of water and salt mass past a cross section during...
H.H. Tanaka
1972, Water Supply Paper 1999-A
Alluvium is the principal aquifer along the Verdigris River between Muskogee and Catoosa, Okla. Yields of 1 to 10 gallons of water per minute, adequate for most domestic and stock uses, are available in almost all areas underlain by alluvium. In places where the proportion of gravel to fine material...
Betsy A. Weld, Kathleen T. Iseri, George W. Brett
1972, Circular 648
Water Resources Division, U.S. Geological Survey
1972, Water Supply Paper 2099
Water Resources Division, U.S. Geological Survey
1972, Water Data Report IL-71-1
Water Resources Division, U.S. Geological Survey
1972, Professional Paper 787
Stanley P. Sauer
1972, Water Supply Paper 1999-L
To determine the reasons for the unusually low runoff in the Concho River basin during the period 1962-68, the physical developments and climatic changes in the basin were identified and related to changes in the regimen of streamflow. Land use, brush infestation, and land-treatment practices have not caused significant changes in...
Robert B. Leonard
1972, Water Supply Paper 1982
Improper disposal of oil-field brine and other wastes has adversely affected the naturally diverse chemical quality of much of the water in the Walnut River basin, south-central Kansas. The basin is an area of about 2,000 square miles in the shape of a rough triangle with its apex toward the...
Harry Stephen Ladd
1972, Professional Paper 532
J. W. M’Gonigle, D.G. Schleicher
1972, IMAP 701
The Plato quadrangle in north-central part of the Moon lies within a series of concentric depressed and raised rings surrounding the Imbrium basin, the center of which lies about 335 km southwest...
B. E. Tucholke, R. N. Oldale, C. D. Hollister
1972, IMAP 716
No abstract available....
Fred Pessl Jr., W. H. Langer
1972, IMAP 784-B
Fred Pessl Jr., C. T. Hildreth
1972, IMAP 784-A
No abstract available....