Geologic reconnaissance of a proposed powersite on the Maksoutof River near Sitka, southeastern Alaska
Alexander A. Wanek
1975, Bulletin 1211-F
Preliminary "steam tables" for NaCl solutions: physical properties of the coexisting phases and thermochemical properties of the H2O component
John L. Haas
1975, Open-File Report 75-674
The August and October 1968 east rift eruptions of Kilauea Volcano, Hawaii
Dallas B. Jackson, D. A. Swanson, R. Y. Koyanagi, T. L. Wright
1975, Professional Paper 890
Water resources data for Arkansas, water year 1974; Part 1, Surface water records
Water Resources Division, U.S. Geological Survey
1975, Water Data Report AR-74-1
Diagenesis and stratigraphy of the Lisburne Group limestones of the Sadlerochit Mountains and adjacent areas, northeastern Alaska
George V. Wood, Augustus K. Armstrong
1975, Professional Paper 857
Cauldron subsidence of Oligocene age at Mount Lewis, northern Shoshone Range, Nevada
Chester T. Wrucke, Miles L. Silberman
1975, Professional Paper 876
No abstract available....
Water resources of the Toppenish Creek Basin, Yakima Indian Reservation, Washington
Water Resources Division, U.S. Geological Survey
1975, Water-Resources Investigations Report 74-42
The Yakima River, which flows along the eastern margin of the Yakima Indian Reservation, provides about 93 percent of the irrigation water for the eastern part of the Toppenish Creek basin--the major agricultural area in the basin . During 1972, the total surface water diverted from all streams and from...
An introduction to the processes, problems, and management of urban lakes
L. J. Britton, R. C. Averett, R. F. Ferreira
1975, Circular 601-K
Lakes are bodies of water formed in depressions on the earth's surface, and as such, act as depositories for a variety of chemical and biological materials. The study of lakes has become increasingly prevalent in recent years. Lakes are a valuable resource, and their multiple uses have made them susceptible...
Sediment transport, turbidity, channel configuration, and possible effects of impoundment of the Mad River, Humboldt County, California
William M. Brown III
1975, Water-Resources Investigations Report 75-26
Sediment-transport conditions were determined at two stations, Mad River near Arcata and Mad River near Kneeland. Using a release-flow model and an empirical equation, the suspended-sediment discharge at Kneeland was estimated to be about 60 percent of the suspended-sediment discharge at the Arcata station. The study of the proposed impoundment...
Geochemical and geologic relations of gold and other elements at the Gold Acres open-pit mine, Lander County, Nevada
Chester T. Wruckle, Theodore J. Armbrustmacher
1975, Professional Paper 860
No abstract available....
Ground-water levels in the United States, 1969-73, Southeastern states
Water Resources Division, U.S. Geological Survey
1975, Water Supply Paper 2171
The potentiometric surface and water quality of the Floridan aquifer; in southwest Hillsborough County, Florida, 1952-74
A. Dan Duerr
1975, Water-Resources Investigations Report 75-50
Large ground-water withdrawals and a 10-year period of below-normal rainfall have caused the potentiometric surface of the Floridan aquifer to decline more than 10 feet (3 metres) in most of a 200-square-mile (520-square-kilometre) area of southwest Hillsborough County (fig. 1). The lowered ground-water levels and the consequent threat of salt-water...
Availability of ground water in the Androscoggin River Basin, northern New Hampshire
John E. Cotton
1975, Water-Resources Investigations Report 75-22
No abstract available. ...
Preliminary photogeologic map of the Chaco Canyon 1 15-minute quadrangle, McKinley County, New Mexico
Willard L. McIntosh
1975, Open-File Report 75-542
No abstract available....
Preliminary photogeologic map of the Cabezon 2 15-minute quadrangle, McKinley and Sandoval Counties, New Mexico
Robert J. Hackman
1975, Open-File Report 75-541
No abstract available....
Analysis of operational plan for Lake Chippewa near Winter, Wisconsin
William R. Krug
1975, Open-File Report 75-487
Historical inflows into Lake Chippewa for 39 years of record were analyzed to determine the possibility of operating the flowage within a 2-foot (0.6-metre) range of stage while maintaining a minimum discharge of 57 cubic feet per second (1.6 cubic metres per second) and limiting the maximum discharge to 7,000...
Potential flood hazard; North Avenue area, Denver Federal Center, Lakewood, Colorado
Richard Ural Grozier, Jerald F. McCain, Louis Ducret
1975, Open-File Report 75-45
No abstract available. ...
Stochastic analysis of particle movement over a dune bed
Baum K. Lee, Harvey E. Jobson
1975, Open-File Report 75-358
Stochastic models are available that can be used to predict the transport and dispersion of bed-material sediment particles in an alluvial channel. These models are based on the proposition that the movement of a single bed-material sediment particle consists of a series of steps of random length separated by rest...
Sandstone geometry, porosity and permeability distribution, and fluid migration in eolian system reservoirs
Robert Lupe, Thomas S. Ahlbrandt
1975, Open-File Report 75-357
Upper Paleozoic to Mesozoic eolian blanket sandstones of the Colorado Plateau and the Rocky Mountains of Colorado and southern Wyoming are texturally complex. As petroleum reservoirs they commonly have poor performance histories. They contain the sediments of a depositional system comprised of three closely associated depositional subenvironments: dune, interdune, and...
Water availability, Elmore County, Alabama
Gregory C. Lines
1975, Open-File Report 75-485
Antimony deposits of Quetta-Pishin District, Quetta Division, Pakistan
F.L. Klinger, John J. Matzko, S.H. Abbas
1975, Open-File Report 75-161
Vein-type deposits of antimony ore, consisting of stibnite and quartz, are found in the hanging wall of faults cutting slate of probable Miocene age 15 miles northeast of Qila Abdullah in the Quetta-Pishin District. The ore is associated with zones of oxidized slate. Although the known deposits are small, the...
Hydrologic effects of reducing irrigation to maintain a permanent pool in John Martin Reservoir, Arkansas River Valley, Colorado
Richard R. Luckey
1975, Open-File Report 75-214
The U.S. Geological Survey has evaluated a plan by the Colorado Division of Wildlife to maintain a permanent pool of 10,000 acre-feet (1.2x107 cubic metres) in John Martin Reservoir on the Arkansas River. The proposed pool would be maintained through the use of water formerly diverted by the Catlin Canal...
Preliminary geologic map of the Wakefield quadrangle, Gogebic County, Michigan
William C. Prinz, Harold A. Hubbard
1975, Open-File Report 75-119
No abstract available....
Generalized logs of drill holes, Sandoval County, New Mexico
Michael N. Machette, George Odell Bachman
1975, Open-File Report 75-643
HYPO71 (revised; a computer program for determining hypocenter, magnitude, and first motion pattern of local earthquakes
William Hung Lee, John C. Lahr
1975, Open-File Report 75-311