Water Resources Division, U.S. Geological Survey
1972, Professional Paper 787
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Publication Extents
Not all publications have extents, not all extents are completely accurateBetsy A. Weld, Kathleen T. Iseri, George W. Brett
1972, Circular 648
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...
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...
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...
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...
Stanley William Lohman
1972, Water Supply Paper 1988
For many years there has been a need for redefinition or more precise definition of certain ground-water terms used in publications by members of the U.S . Geological Survey. Another problem has been the expression of the coefficient of permeability (herein redefined as hydraulic conductivity) and the coefficient of transmissibility...
F. A. Kilpatrick, T. Ray Cummings
1972, Water Supply Paper 1586-J
A tracer study was conducted in Port Royal Sound to simulate the movement and ultimate pattern of concentration of a solute continuously injected into the flow. A total of 750 pounds of Rhodamine WT dye was injected by boat during a period of 24.8 hours in a line across the...
Terry W. Offield
1972, IMAP 626
The Flamsteed K region is in the southern part of Oceanus Procellarum, approximately 60 km (kilometers) north of the crater Flamsteed<span class="NormalTextRun SCXW187090825...
Henry W. Roehler
1972, Geologic Quadrangle 1019
Don Price
1972, IMAP 591-M
The general availability of ground water was determined from well records collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies. Data are for aquifers that in most places are less than 1,000 feet below the land surface. In areas of few or no wells, potential well...
Henry W. Roehler
1972, Geologic Quadrangle 1001
Fred Pessl Jr., C. T. Hildreth
1972, IMAP 784-A
No abstract available....
Don Price
1972, IMAP 591-K
The general chemical quality of water was determined from quality-of-water data collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies. Sources of data include springs, and wells that tap aquifers at depths of less than 1,000 feet. In areas where quality-of-water data are inadequate or lacking,...
D. H. Scott, H. A. Pohn
1972, IMAP 799
The Macrobius quadrangle is in the northeast quadrant of the Moon’s near side. Although predominantly a highland area centered around the Taurus Mountains (Montes Taurus), it is bounded by...
G. R. Scott
1972, IMAP 790-D
No abstract available....
D.W. Rankin, G.H. Espenshade, R. B. Neuman
1972, IMAP 709-A
G. R. Scott
1972, IMAP 790-F
No abstract available....
K.M. Waddell, Don Price
1972, Hydrologic Atlas 417
The United States Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Water Rights, began a reconnaissance in 1967 to obtain essential water-quality information for the Bear River basin. The reconnaissance was directed toward defining the chemical quality of the basin’s surface waters, including suitability for...
P. W. Schmidt, J. C. Reed Jr.
1972, IMAP 786-E
D.F. Barnes
1972, Open-File Report 72-17
G. R. Scott
1972, IMAP 790-E
J. C. Reed Jr., J. R. Keith
1972, IMAP 786-B
H. A. Pohn
1972, IMAP 713
The Tycho quadrangle is centrally located in the southern half of the earthside hemisphere of the Moon. The area is characterized by a high density of craters, the largest of which <span...
T.A. Mutch, R.S. Saunders
1972, IMAP 702
The Hommel quadrangle is in the southeast highlands of the earthside hemisphere of the Moon. The major geologic units are smooth and ridged <span class="NormalTextRun SCXW160887891...