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Page 5389, results 134701 - 134725

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Populations, feeding ecology and molt of Steller's Eiders
Margaret R. Petersen
1981, The Condor (83) 256-262
This study considers the temporal and spatial distribution of Steller's Eiders (Polysticta stelleri) during molt along the north side of the Alaska Peninsula from Port Heiden to Bechevin Bay. Subadult eiders molted primarily at Nelson Lagoon, adult males at Nelson Lagoon and Izembek Bay, and adult females primarily at Izembek...
Thermodynamic tabulations for selected phases in the system CaO-Al2O3-SiO2-H2 at 101.325 kPa (1 atm) between 273.15 and 1800 K
John L. Haas Jr., Glipin R. Robinson Jr., Bruch S. Hemingway
1981, Journal of Physical and Chemical Reference Data (10) 575-670
The standard thermodynamic properties of phases in the lime‐alumina‐silica‐ water system between 273.15 and 1800 K at 101.325 kPa (1 atm) were evalated from published experimental data. Phases included in the compilation are boehmite, diaspore, gibbsite, kaolinite, dickite, halloysite, andalusite, kyanite, sillimanite, Ca‐Al cliniopyroxene, anorthite, gehlenite, grossular, prehnite, zoisite, margarite,...
Reconnaissance geochemical survey of gully and stream sediments, and geologic summary, in part of the Okanogan Range, Okanogan County, Washington
C. Dean Rinehart
1981, Bulletin 74
A reconnaissance geochemical stream-sediment sampling survey was conducted in a 1,150-km2 (440 mi2) area in the central part of the Okanogan Range, adjacent on the west to a 2,000-km2 (800 mi2) area previously studied. About 75 percent of the bedrock is composed of a mosaic of elongate northwest-trending Mesozoic plutons,...
Hydrology and model of North Fork Solomon River Valley, Kirwin Dam to Waconda Lake, north-central Kansas
Donald G. Jorgensen, Lloyd E. Stullken
1981, Irrigation Series 6
The alluvial valley of the North Fork Solomon River is an important agricultural area. Reservoir releases diverted below Kirwin Dam are the principal source of irrigation water. During the 1970'S, severe water shortages occurred in Kirwin Reservoir and other nearby reservoirs as a result of an extended drought. Some evidence...
Integrated uranium system in the Marysvale volcanic field, west-central Utah
T. A. Steven, C. G. Cunningham, M. N. Machette
1981, Book chapter, Uranium in volcanic and volcaniclastic rocks
Uranium in the Marysvale volcanic field is known to occur in several geologic environments and is thought to occur in others. These known and hypothetical occurrences are of various kinds, ranging in derivation from rhyolite magma, through porphyry-type deposits, hydrothermal vein deposits, dispersed hydrothermal deposits, and, after secondary transport in...
Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake
William B. Joyner, David M. Boore
1981, Bulletin of the Seismological Society of America (71) 2011-2038
We have taken advantage of the recent increase in strong-motion data at close distances to derive new attenuation relations for peak horizontal acceleration and velocity. This new analysis uses a magnitude-independent shape, based on geometrical spreading and anelastic attenuation, for the attenuation curve. An innovation in technique is introduced that...
Water resources of the Kisatchie well-field area near Alexandria, Louisiana
James E. Rogers
1981, Water Resources Technical Report 26
Sands of Miocene, Pliocene(?), and Pleistocene age contain fresh-water in central Rapides Parish, La. In this area the base of fresh ground water ranges from 900 feet to more than 2,500 feet below National Geodetic Vertical Datum of 1929. The principal sources of water are the Carnahan Bayou, Williamson Creek,...
Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma
Donald L. Hart Jr., Robert E. Davis
1981, Circular 81
The Antlers aquifer, which consists of as much as 900 feet of friable sandstone, silt, clay, and shale, crops out in an area of 1,860 square miles and underlies about 4,400 square miles in southeastern Oklahoma. Precipitation ranges from 35 to 50 inches per year across the outcrop area, which...
Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico
Clyde A. Wilson, Robert R. White, Brennon R. Orr, R. Gary Roybal
1981, Technical Report 43
The Rincon and Mesilla Valleys of New Mexico extend from Caballo Reservoir to El Paso del Norte, west of El Paso, Texas. Water supplies for this area are obtained from the Rio Grande and from the saturated sediments filling the intermontane basins of south-central New Mexico.The two major aquifers are...