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Page 4158, results 103926 - 103950

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Radon anomalies on three kinds of faults in California
C.-Y. King, W. Zhang, B.-S. King
1993, Pure and Applied Geophysics PAGEOPH (141) 111-124
Radon emanation is known to be anomalously high along active faults in many parts of the world. We tested this relationship in California during July and early August 1992, using a portable radonmeter to conduct soil-air radon surveys at 5 sites across three kinds of faults: Creeping, locked, and freshly...
A finite-volume Eulerian-Lagrangian Localized Adjoint Method for solution of the advection-dispersion equation
R. W. Healy, T.F. Russell
1993, Water Resources Research (29) 2399-2413
A new mass-conservative method for solution of the one-dimensional advection-dispersion equation is derived and discussed. Test results demonstrate that the finite-volume Eulerian-Lagrangian localized adjoint method (FVELLAM) outperforms standard finite-difference methods, in terms of accuracy and efficiency, for solute transport problems that are dominated by advection. For dispersion-dominated problems, the performance...
Slumgullion; Colorado’s natural landslide laboratory
L.M. Highland
1993, Earthquakes & Volcanoes (USGS) (24) 208-221
The mammoth Slumgullion landslide in southwestern Colorado is the largest actively moving landslide in Colorado and, perhaps, the entire country. To learn more about how and why landslides move the way they do, scientists at the U.S Geological Survey (USGS) have observed and monitored the remarkably regular movement of this...
Seismic detection of tornadoes
F. B. Tatom
1993, Earthquakes & Volcanoes (USGS) (24) 222-234
Tornadoes represent the most violent of all forms of atmospheric storms, each year resulting in hundreds of millions of dollars in property damage and approximately one hundred fatalities. In recent years, considerable success has been achieved in detecting tornadic storms by means of Doppler radar. However, radar systems cannot determine...
The Golden bypass landslide, Golden, Colorado
L.M. Highland, W. M. Brown III
1993, Earthquakes & Volcanoes (USGS) (24) 4-14
Slope instability along a new highway bypass in Golden, Colorado, became a major concern in 1993. Rains and snowmelt accelerated movement of a landslide that had begun to develop before the bypass was opened to traffic in July of 1991. The downslope movement of earth materials increased significantly in 1993. During...
Antarctic glacier-tongue velocities from Landsat images: First results
Baerbel K. Lucchitta, K.F. Mullins, A.L. Allison, Jane G. Ferrigno
1993, Annals of Glaciology (17) 356-366
We measured the velocities of six glacier tongues and a few tongues within ice shelves distributed around the Antarctic coastline by determining the displacement of crevasse patterns seen on sequential Landsat images. The velocities range from less than 0.2 km a−1 for East Antarctic ice-shelf tongues to more than 2.5...
Sensitivity of juvenile striped bass to chemicals used in aquaculture
Terry D. Bills, Leif L. Marking, George E. Howe
1993, Resource Publication 192
Efforts to restore anadromous striped bass (Morone saxatilis) populations by the U.S. Fish and Wildlife Service and other agencies over the past 20 years have concentrated on hatchery culture to supplement dwindling natural reproduction. Adult fish captured for artificial spawning are stressed by handling and crowding in...
Borehole techniques identifying subsurface chimney heights in loose ground-some experiences above underground nuclear explosions
R. D. Carroll, J.W. Lacomb
1993, International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts (30) 575-590
The location of the subsurface top of the chimney formed by the collapse of the cavity resulting from an underground nuclear explosion is examined at five sites at the Nevada Test Site. The chimneys were investigated by drilling, coring, geophysical logging (density, gamma-ray, caliper), and seismic velocity surveys. The identification...
Geological and technological assessment of artificial reef sites, Louisiana outer continental shelf
D.L. Pope, T.F. Moslow, J.B. Wagner
1993, Ocean and Coastal Management (20) 121-145
This paper describes the general procedures used to select sites for obsolete oil and gas platforms as artificial reefs on the Louisiana outer continental shelf (OCS). The methods employed incorporate six basic steps designed to resolve multiple-use conflicts that might otherwise arise with daily industry and commercial fishery operations, and...
Effects of agricultural nutrient management on nitrogen fate and transport in Lancaster County, Pennsylvania
D. W. Hall, D. W. Risser
1993, Water Resources Bulletin (29) 55-76
Nitrogen inputs to, and outputs from, a 55-acre site in Lancaster County, Pennsylvania, were estimated to determine the pathways and relative magnitude of loads of nitrogen entering and leaving the site, and to compare the loads of nitrogen before and after the implementation of nutrient management. Inputs of nitrogen to...
Seasonal prevalence of Clostridium botulinum type C in the sediments of the northern California wetland
Renee J. Sandler, Tonie E. Rocke, M.D. Samuel, Thomas M. Yuill
1993, Journal of Wildlife Diseases (29) 533-539
The prevalence of Clostridium botulinum type C (% of positive sediment samples) was determined in 10 marshes at Sacramento National Wildlife Refuge (SNWR), located in the Central Valley of California (USA), where avian botulism epizootics occur regularly. Fifty-two percent of 2,200 sediment samples collected over an 18-mo period contained C....
Advection and diffusion in a variable-salinity confining layer
Leonard F. Konikow, Javier Rodriguez Arevalo
1993, Water Resources Research (29) 2747-2761
A numerical model that simulates groundwater flow and solute transport for cases in which fluid properties are variable was applied in one dimension (vertical) to the shallow, low-permeability, clayey, confining layer in Doñana National Park in southwestern Spain. The salinity in the 80-m-thick confining layer decreases from a brine near...
The system controlling the composition of clastic sediments
Mark J. Johnsson
1993, Special Paper of the Geological Society of America (284) 1-20
The composition of clastic sediments and rocks is controlled by a complex suite of parameters operating during pedogenesis, erosion, transport, deposition, and burial. The principal first-order parameters include source rock composition, modification by chemical weathering, mechanical disaggregation and abrasion, authigenic inputs, hydrodynamic sorting, and diagenesis. Each of these first-order parameters...
Digestion of larval American shad by cyprinids
D. V. Rottiers, J. H. Johnson
1993, Ecology of Freshwater Fish (2) 147-151
Cyprinids have pharyngeal teeth for grinding food before swallowing and a continuous gut with no discrete stomach. This digestive tract structure, as well as the feeding behavior traits shown by cyprinids, makes it difficult to identify and measure the amount of food consumed by these fishes. The relations among quantity...
Isolates of viral hemorrhagic septicemia virus from North America and Europe can be detected and distinguished by DNA probes
W.N. Batts, C.K. Arakawa, J. Bernard, J. R. Winton
1993, Diseases of Aquatic Organisms (17) 67-71
Biotinylated DNA probes were constructed to hybndize with speclfic sequences within the messenger RNA (mRNA) of the nucleoprotein (N) gene of vlral hemorrhagic septicemia virus (VHSV) reference strains from Europe (07-71) and North Arnenca (Makah) Probes were synthesized that were complementary to (1) a 29-nucleotide sequence near the center of...
Considerations and applications of the illite/smectite geothermometer in hydrocarbon-bearing rocks of Miocene to Mississippian age
Richard M. Pollastro
1993, Clays and Clay Minerals (41) 119-133
Empirical relationships between clay mineral transformations and temperature provide a basis for the use of clay minerals as geothermometers. Clay-mineral geothermometry has been applied mainly to diagenetic, hydrothermal, and contact- and burial-metamorphic settings to better understand the thermal histories of migrating fluids, hydrocarbon source beds, and ore and mineral formation.Quantitatively,...
Preliminary results from an isotope hydrology study of the Kilauea Volcano area, Hawaii
M. A. Scholl, C. J. Janik, S. E. Ingebritsen, J.P. Kauathikaua, F. A. Trusdell
Anon, editor(s)
1993, Conference Paper, Transactions - Geothermal Resources Council
Deuterium (D) content of groundwater and precipitation, and tritium content of selected groundwater samples are used to infer flowpaths for groundwater in the Kilauea Volcano area. The spatial distribution of calculated recharge elevations and residence times for groundwater samples tends to support the idea that Kilauea's rift zones comprise leaky...
Conservation genetics of managed ungulate populations
Kim T. Scribner
1993, Acta Theriologica (38) 89-101
Natural populations of many species are increasingly impacted by human activities. Perturbations are particularly pronunced for large ungulates due in part to sport and commercial harvest, to reductions and fragmentation of native habitat, and as the result of reintroductions. These perturbations affect population size, sex and age composition, and population...
New geophysical models related to heat sources in the geysers-clear lake region, California
W. D. Stanley, R.J. Blakely
Anon, editor(s)
1993, Conference Paper, Transactions - Geothermal Resources Council
We present an updated view of the geological and geophysical complexities of the upper crust in The Geysers-Clear Lake region in order to provide additional information regarding local structures and possible heat sources. New models and ideal-body analysis of the gravity data, new electromagnetic sounding models, and arguments made from...
Wind and tidal forcing of a buoyant plume, Mobile Bay, Alabama
R. P. Stumpf, G. Gelfenbaum, J.R. Pennock
1993, Continental Shelf Research (13) 1281-1301
AVHRR satellite imagery and in situ observations were combined to study the motion of a buoyant plume at the mouth of Mobile Bay, Alabama. The plume extended up to 30 km from shore, with a thickness of about 1 m. The inner plume, which was 3-8 m thick, moved between...