Melvin D. Edwards
1975, Open-File Report 74-1029
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Page 5493, results 137301 - 137325
Publication Extents
Not all publications have extents, not all extents are completely accurateAndrew Brown, Irving May
1975, Open-File Report 75-135
The Geological Survey?s investigations of the Chattanooga shale in Tennessee and adjacent states on behalf of the U.S. Atomic Energy Commission consisted mostly of geologic studies and routine analyses of samples for uranium. In the course of the studies, however, other investigations were made, primarily to find answers to specific...
G. L. Loelkes (compiler), I.L. Hardin, E.C. Napier, M.J. Chambers, Eldon Jessen, R.A. Johnson
1975, Open-File Report 75-235
Hugo B. Fischer, J.D. Stoner, W.L. Haushild, J. B. McConnell
1975, Professional Paper 917
G. L. Loelkes (compiler), I.L. Hardin, E.C. Napier, M.J. Chambers, Eldon Jessen, R.A. Johnson
1975, Open-File Report 75-222
Water Resources Division, U.S. Geological Survey
1975, Water Data Report ID-74-2
Dewey Harold Amos
1975, Open-File Report 75-17
R.E. Hansen
1975, Open-File Report 75-88
Ted G. Theodore, David W. Blake
1975, Open-File Report 75-593
Wilfred James Carr, Donald E. Trimble
1975, Open-File Report 75-326
Stanley J. Luft
1975, Open-File Report 75-116
William Scott Parks
1975, Open-File Report 75-586
Water Resources Division, U.S. Geological Survey
1975, Open-File Report 75-52
K. L. Pierce, P. W. Schmidt
1975, Miscellaneous Field Studies Map 695
No abstract available....
W. F. Hardt, F. H. Olmsted, Frank W. Trainer
1975, Open-File Report 76-429
Charles A. Pascale
1975, Open-File Report 74-256
R. W. Page
1975, Open-File Report 75-315
The Fresno northeast area includes about 133 square miles (344 square kilometres) in the central part of California. Four physiographic units occur in the area, the largest of which is the compound alluvial fan of the intermittent streams north of the Kings River.Geologic units consist of consolidated rocks and unconsolidated...
Wilfred P. Hasbrouck, M.L. Botsford, W.P. Jennings
1975, Open-File Report 75-97
A high-quality ground magnetic survey was conducted over the Ralston dike, Jefferson County, Colorado, from September 1973 to June 1974. The data obtained on this survey are tabulated in this report....
Water Resources Division, U.S. Geological Survey
1975, Water Data Report NE-74-2
No abstract available. ...
Water Resources Division, U.S. Geological Survey
1975, Water Data Report MO-74-1
Water resources data for the 1974 water year for Missouri including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included...
Water Resources Division, U.S. Geological Survey
1975, Water Data Report AR-74-2
John G. Newton, Jerald F. McCain, James D. Turner
1975, Open-File Report 75-476
Large quantities of ground water and surface water are available in Washington County. Major sources of ground water are the Gosport Sand and Lisbon Formation undifferentiated, the Miocene Series undifferentiated, and alluvium and low terrace deposits. The Miocene, the most productive source of ground water, will yield 0.5 to 1.0...
Gerald K. Moore, Morris Deutsch
1975, Ground Water (13) 214-226
ERTS imagery offers the first opportunity to apply moderately high-resolution satellite data to the nationwide study of water resources. This imagery is both a tool and a form of basic data. Like other tools and basic data, it should be considered for use in ground-water investigations. The main advantage of...
Timothy C. Bidwell
1975, Photogrammetric Engineering and Remote Sensing (41) 1273-1284
Research in remote-sensing applications has increased dramatically since the launch of the Earth Resources Technology Satellite-l (ERTS-l, renamed LANDSAT-I) and Skylab's Earth Resources Experiment Package (EREP). It is becoming increasingly more difficult to keep abreast of university research publications related to remote sensing. To assist researchers in locating those universities...
Eugene C. Robertson
1975, Report
The center of the Earth lies nearly 4,000 miles beneath our feet. At present the nature of the Earth's interior is known only from indirect evidence collected from studies of rocks and minerals, seismic waves, heat flow from the interior, and the Earth's gravity and magnetic field and through comparisons...