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Not all publications have extents, not all extents are completely accurate
Water resources of the Milford area, Utah, with emphasis on ground water
R. W. Mower, R.M. Cordova
1974, Technical Publication 43
The investigation of the water resources of the Milford area was made as part of a cooperative program with the Utah Department of Natural Resources, Division of Water Rights, to investigate the water resources of the State. The primary purpose of this report is to provide basic hydrologic information needed...
Limnological data from selected lakes in the San Francisco Bay region, California
Linda J. Britton, Rodger F. Ferreira, Robert C. Averett
1974, Open-File Report 3019-27
Limnological data were compiled on 21 lakes in the San Francisco Bay area. The data were obtained from regulating agencies and from recent surveys made by the U.S. Geological Survey. The history of each lake and of its respective regulating agency is presented, along with methods used for data collection...
Evaluation of hydraulic characteristics of a deep artesian aquifer from natural water-level fluctuations, Miami, Florida
Frederick W. Meyer
1974, Florida Bureau of Geology Report of Investigations 75
Knowledge of tho hydraulic characteristics of aquifer systems is fundamental to defining the vertical and horizontal controls on fluid movement, information which is needed for assessing the environmental impact of subsurface waste storage. To meet this objective, natural water-level fluctuations in the 2,947-foot deep Peninsula Utilities disposal well near Miami,...
The availability of water in the Little Lost River Basin, Idaho
Alfred Clebsch Jr., H.A. Waite, S.O. Decker
1974, Water Information Bulletin 37
The Little Lost River basin, an elongated, northwest trending structurally formed intermontane valley, drains an area of about 900 square miles into a closed depression near the northwestern edge of the Snake River Plain. Runoff from snowmelt and rainfall on the Lost River Range on the west and the Lemhi...
A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area
E. G. Crosthwaite
1974, Water Information Bulletin 38
Direct-current resistivity soundings and exploratory drilling suggest that the basalt of the Snake River Group is relatively thin in the area along the Snake River that is topographically suitable for pumping large quantities of ground water in exchange for surface water. The formations underlying the Snake River Group appear to...
Analyses and economic potential of monazite in Liberia
Sam Rosenblum
1974, Journal of Research of the U.S. Geological Survey (2) 689-692
Eleven monazite samples from Liberia, including seven from beach sands, were analyzed by the X-ray fluorescence method. The monazite samples, containing only one-half percent impurities, were obtained by use of a hot Clerici-solution procedure for purification which was devised by the author. The percentage of the rare-earth elements in Liberian...
Apollo 11 voice transcript pertaining to the geology of the landing site
N. G. Bailey, G. E. Ulrich
1974, Report
On July 20, 1969, America's Eagle touched down in southwestern Mare Tranquillitatis beginning man's firsthand exploration of the moon. This document is an edited record of the conversations between astronauts Neil Armstrong and Edwin "Buzz" Aldrin, Jr., at Tranquility Base, and Bruce McCandless at Mission Control in Houston during the...
Geology and mineral deposits of Churchill County, Nevada
Ronald Willden, Robert C. Speed
1974, NBMG Bulletin 83
Churchill County, in west-central Nevada, is an area of varied topography and geology that has had a rather small total mineral production. The western part of the county is dominated by the broad low valley of the Carson Sink, which is underlain by deposits of Lake Lahontan. The bordering mountain...
Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras
R.E. Mattick, R. Q. Foote, N. L. Weaver, M. S. Grim
1974, American Association of Petroleum Geologists Bulletin (58) 1179-1190
To assess the area’s hydrocarbon potential, regional geologic and geophysical studies are being conducted by the U.S. Geological Survey to determine the structural framework of the United States Atlantic outer continental shelf (AOCS) north of Cape Hatteras. Preliminary interpretations of geophysical data suggest that the buried ridge under the eastern...
Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley
Water Resources Division, U.S. Geological Survey
1974, Water Data Report CA-73-1-2
Surface-water records for the 1973 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report, Records for a few pertinent gaging stations in bordering States also are included, The records were collected and computed by the...
Water resources inventory of Connecticut Part 5: lower Housatonic River basin
William E. Wilson, Edward L. Burke, Chester E. Thomas Jr.
1974, Connecticut Water Resources Bulletin 19
The 557 square miles of the lower Housatonic River basin in western Connecticut include the basins of two major tributaries, the Pomperaug and Naugatuck Rivers. Nearly all water is derived from precipitation, which averaged 47 inches per year during 1931-60, In this period an additional 570 billion gallons of water...