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Page 5330, results 133226 - 133250

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Hydrologic data for Cow Bayou, Brazos River Basin, Texas, 1975
R.N. Mitchell, E.E. Wehmeyer
1977, Open-File Report 76-723
The U.S. Soil Conservation Service is actively engaged in the implementation of flood- and soil-erosion reducing measures in Texas under the authority of. "The Flood Control Act of 1936 and 1944" and "Watershed Protection and Flood Prevention Act" (Public Law 566), as amended. The Soil Conservation Service has found a...
Progress report on uranium investigations in the Zane Hills area, west-central Alaska
Thomas P. Miller, Raymond L. Elliott
1977, Open-File Report 77-428
The Zane Hills pluton underlies a mountainous area of about 460 km2 in west-central Alaska and is locally enriched in uranium and thorium (Miller and Ferrians, 1968; Miller, 1970; Staatz and Miller, 1976). While over 90 percent of the pluton consists of granodiorite with average contents of uranium and thorium,...
Preliminary geologic map of Seward Peninsula, Alaska
Travis Hudson
1977, Open-File Report 77-167-A
This preliminary map is the first of several data compilations being prepared as a foundation for evaluating the mineral resource potential of Seward Peninsula. In addition to the sources of geologic data credited in the index map, Sainsbury's recent (1975) summary of his extensive geologic studies on Seward Peninsula has...
Evaporation and radiation measurements at Salton Sea, California
Alex M. Sturrock
1977, Open-File Report 77-74
Evaporation from the Salton Sea, Calif., was computed for a 539-day period between July 14, 1967, and January 2, 1969, by use of energy-budget, mass-transfer, and water budget methods. The total evaporation computed by the three methods agreed within 5 percent. The values of heat transfer to and from the...
The biostratigraphy and paleoecology of the Gerster limestone (Upper Permian) in Nevada and Utah
Bruce R. Wardlaw
1977, Open-File Report 77-470
The Gerster Limestone contains three minor lithofacies: the packstone, wackestone, and mixed facies, differentiated largely on the basis of the carbonate matrix and mud content of the rocks. Five biostratigraphic zones ranging in age from Roadian-Wordian to Wordian are, in ascending order, the Thamnosia, Kuvelousia, transition, Yakovlevia, and upper zones....
Biostratigraphic zonation of the Park City Group
Bruce R. Wardlaw, James W. Collinson
1977, Open-File Report 77-853
Five biostratigraphic zones based on the distribution of brachiopods and conodonts are proposed for the Park City Group. They are: the Peniculauris ivesi-Neostreptognathodus prayi Zone, the Peniculauris bassi-Neostreptognathodus sulcoplicatus Zone, the Peniculauris bassi-Neostreptognathodus sp. C Zone, the Thamnosia depressa Zone, and the Yakovlevia multistriata-Neogondolella bitteri Zone. They range in age...
Surficial and applied surficial geology of the Belchertown Quadrangle, Massachusetts
Joseph A. Caggiano
1977, Open-File Report 77-633
Till and stratified drift overlie maturely dissected topography in the Belchertown quadrangle, an area that straddles the New England Upland and Connecticut Valley Lowland in central Massachusetts. Lower Paleozoic, massive quartzo-feldspathic gneiss, quartzite and schist of the Pelham dome and Devonian granodiorite and quartz diorite of the Belchertown intrusive complex...
Structural and heat-flow implications of infrared anomalies at Mt. Hood, Oregon
Jules D. Friedman, David Frank
1977, Open-File Report 77-599
Surface thermal features occur in an area of 9700 m2 at Mt. Hood, on the basis of an aerial line-scan survey made April 26, 1973. The distribution of the thermal areas below the summit of Mt. Hood, shown on planimetrically corrected maps at 1:12,000, suggests structural control by a fracture...