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Page 5930, results 148226 - 148250

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California
Earl E. Brabb
1964, American Association of Petroleum Geologists Bulletin (48) 670-679
The San Lorenzo Formation was for many years considered synonymous with Oligocene Series. The formation name was extended, incorrectly in most cases, to rocks as far north as British Columbia and as far south as southern California. The formation in its type area was never adequately studied, resulting in fallacious...
Geology and ground-water resources of the Jordan Valley, Utah
I. Wendell Marine, Don Price
1964, Utah Geological and Mineralogical Survey Water-Resources Bulletin 7
The Jordan Valley occupies about 400 square miles in the central part of Salt Lake County in north-central Utah. Salt Lake City, the capital of Utah, is in the northeastern part of the valley. The valley is at the eastern margin of the Basin and range physiographic province, and it...
Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report
D. C. Hahl, R.H. Langford
1964, Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-II
During the 1960 and 1961 water years an annual load of about 2 million tons of dissolved minerals was contributed to the Great Salt Lake area by surficial sources. Almost 60 percent of this load was sodium and chloride. Of the six units contributing to the lake area, three -...
Developing a state water plan: Ground-water conditions in Utah, spring of 1964
Ted Arnow, R.G. Butler, R. W. Mower, Joseph S. Gates, R.M. Cordova, C.H. Carpenter, L.J. Bjorklund, R.D. Feltis, G.B. Robinson, G. W. Sandberg
1964, Cooperative Investigations Report 2
This report is the first in a series of annual reports which will describe ground-water conditions in Utah. It was prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and was designed to provide the data for interested parties, such as legislators, administrators, and planners...
The role of free and bound water in irradiation preservation: Free radical damage as a function of the physical state of water
Gary Wedemeyer, A.M. Dollar
1964, Journal of Food Science (29) 525-529
English sole fillets previously equilibrated with aqueous 0.1% cysteine were dehydrated by three methods to moisture levels ranging from 2 to 72%. Model systems using cellulose to replace the fish tissue were also used. The samples were irradiated at 1 Mrad in an air, nitrogen, or oxygen atmosphere. The destruction...
A preliminary summary of a seismic-refraction survey in the vicinity of the Tonto Forest Observatory, Arizona
J.C. Roller, W. H. Jackson, D. H. Warren, J. H. Healy
1964, Crustal Studies Technical Letter 23
The U.S. Geological Survey complete d a seismic-refraction survey in the vicinity of the Tonto Forest Seismological Observatory (T.F.S.O.) in April and May 1964. More than 1200 km of reversed profiles were surveyed to determine the crustal structure and crustal and upper mantle velocities in this area. The purpose of...
Seismic-refraction measurements of crustal structure between American Falls Reservoir, Idaho, and Flaming Gorge Reservoir, Utah
Ronald Willden
1964, Crustal Studies Technical Letter 21
Interpretation of a reversed seismic-refraction profile recorded between American Falls reservoir and Flaming Gorge reservoir in May 1963 indicates that the depth to the Mohorovicic discontinuity is about 31 km at American Falls and 37 km at Flaming Gorge. The existence of an intermediate crustal layer at a depth of...
Crustal structure between Lake Mead, Nevada, and Mono Lake, California
Lane R. Johnson
1964, Crustal Studies Technical Letter 22
Interpretation of a reversed seismic-refraction profile between Lake Mead, Nevada, and Mono Lake, California, indicates velocities of 6.15 km/sec for the upper layer of the crust, 7.10 km/sec for an intermediate layer, and 7.80 km/sec for the uppermost mantle. Phases interpreted to be reflections from the top of the intermediate...