Water Resources Division, U.S. Geological Survey
1972, Water Data Report GA-71-1
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Publication Extents
Not all publications have extents, not all extents are completely accurateEdward Huntington Cobb
1972, Miscellaneous Field Studies Map 437
William D. Johnson, Avery E. Smith
1972, Geologic Quadrangle 995
Water Resources Division, U.S. Geological Survey
1972, Geophysical Investigations Map 834
Donald A. Myers, E. J. McKay
1972, Geologic Quadrangle 1008
William D. Johnson
1972, Geologic Quadrangle 1045
Charles Reynolds Warren
1972, Geologic Quadrangle 984
T. H. Nilsen
1972, Miscellaneous Field Studies Map 321
Paul E. Soister
1972, Geologic Quadrangle 875
Water Resources Division, U.S. Geological Survey
1972, Water Data Report CT-71-1
Stanley J. Luft
1972, Geologic Quadrangle 1037
Thomas P. Miller, Donald Grybeck, Raymond L. Elliott, Travis Hudson
1972, Open-File Report 72-256
No abstract available....
R. L. Detterman (compiler), E.H. Cobb
1972, Miscellaneous Field Studies Map 364
E. H. Cobb
1972, Miscellaneous Field Studies Map 391
R.R. Burchett, V. H. Dreeszen, E.C. Reed, G.E. Prichard
1972, IMAP 729
Water Resources Division, U.S. Geological Survey
1972, Water Data Report AZ-71-2
Edward E. McGregor, J. Mark Cattermole
1972, Open-File Report 72-240
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...
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...
Water Resources Division, U.S. Geological Survey
1972, Water Data Report AR-71-2
Water Resources Division, U.S. Geological Survey
1972, Professional Paper 787
Betsy A. Weld, Kathleen T. Iseri, George W. Brett
1972, Circular 648
Water Resources Division, U.S. Geological Survey
1972, Water Supply Paper 2099
Henry Trapp Jr.
1972, Open-File Report 72-381