Publications
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Temperature, snowmelt, and the onset of spring season landslides in the central Rocky Mountains Temperature, snowmelt, and the onset of spring season landslides in the central Rocky Mountains
Snow meltwater (snowmelt) that seeps into the subsurface is a major factor contributing to the development of landslides during the spring in mountainous areas of the Rocky Mountain region. An examination of historical temperature data in relation to spring season landslide occurrences reveals an association between the landslide events and intervals of rising temperatures that...
Authors
Alan F. Chleborad
The Coastal and Marine Geology Program of the U.S. Geological Survey The Coastal and Marine Geology Program of the U.S. Geological Survey
Nearly half of all Americans live within an hour's drive of an ocean, the Gulf of Mexico, or the Great Lakes. The U.S. coastal oceans are an economically vital transportation, commercial and recreational resource. They provide food, energy, and minerals for the entire Nation: on a global scale, they harbor critical habitat for important animal and plant species.
Authors
S. Jeffress Williams
Composition of the crust in the Grenville and Appalachian Provinces of North America inferred from VP/VS ratios Composition of the crust in the Grenville and Appalachian Provinces of North America inferred from VP/VS ratios
We use the ratios between P and S wave velocities (VP/VS), derived from seismic refraction data, to infer the composition of the crust in the Grenville and the Appalachian Provinces of North America. The crust exhibits VP/VS increasing with depth from 1.64 to 1.84; there is a clear distinction between the Grenville Province (average VP/VS=1.81) and the Appalachian Province (average VP/VS...
Authors
G. Musacchio, Walter D. Mooney, James H. Luetgert, Nikolas I. Christensen
The variability of PSV response spectra across a dense array deployed during the Northridge aftershock sequence The variability of PSV response spectra across a dense array deployed during the Northridge aftershock sequence
This study addresses the variability of pseudo-velocity response spectra across an array deployed on stiff soil in the San Fernando Valley during the Northridge (Mw 6.7) aftershock sequence. The separation between stations ranged from 0.5 to 5 km, and the aftershock magnitudes ranged from 2.3 to 4.0. We find that 95-percent of observed response spectra are within a factor of 1.9 to 2.6...
Authors
Edward H. Field, Susan E. Hough
Water-level changes in response to the 20 December 1994 earthquake near Parkfield, California Water-level changes in response to the 20 December 1994 earthquake near Parkfield, California
We analyze co-seismic changes of water level in nine wells near Parkfield, California, produced by an MD 4.7 earthquake on 20 December 1994 in order to test the hypothesis that co-seismic water-level changes are proportional to co-seismic volumetric strain. For each well, a quantitative relationship between water level and volumetric strain can be inferred from water-level fluctuations...
Authors
Eddie Quilty, Evelyn A. Roeloffs
The imager for Mars Pathfinder experiment The imager for Mars Pathfinder experiment
The imager for Mars Pathfinder (IMP), a stereoscopic, multispectral camera, is described in terms of its capabilities for studying the Martian environment. The camera's two eyes, separated by 15.0 cm, provide the camera with range‐finding ability. Each eye illuminates half of a single CCD detector with a field of view of 14.4×14.0° and has 12 selectable filters. The ƒ/18 optics have a...
Authors
P. H. Smith, M.G. Tomasko, D. Britt, D.G. Crowe, R. Reid, H.U. Keller, N. Thomas, F. Gliem, P. Rueffer, R. Sullivan, R. Greeley, J. M. Knudsen, M.B. Madsen, H.P. Gunnlaugsson, S.F. Hviid, W. Goetz, Laurence A. Soderblom, L. Gaddis, Randolph L. Kirk
Natural disasters: forecasting economic and life losses Natural disasters: forecasting economic and life losses
Events such as hurricanes, earthquakes, floods, tsunamis, volcanic eruptions, and tornadoes are natural disasters because they negatively impact society, and so they must be measured and understood in human-related terms. At the U.S. Geological Survey, we have developed a new method to examine fatality and dollar-loss data, and to make probabilistic estimates of the frequency and...
Authors
Stuart P. Nishenko, Christopher C. Barton
Some comparisons between recent ground-motion relations Some comparisons between recent ground-motion relations
We provide an overview of new ground-motion relations for eastern North America (ENA) developed over the last five years. The empirical-stochastic relations of Atkinson and Boore (1995) are compared to relations developed by the Electric Power Research Institute (EPRI, 1993; also Toro et al., 1994), Frankel et al. (1996), and the consensus ENA ground-motion values as reported by SSHAC...
Authors
Gail M. Atkinson, David Boore
Physiography, Geomorphic/geologic Mapping and Stratigraphy of Venus Physiography, Geomorphic/geologic Mapping and Stratigraphy of Venus
No abstract available.
Authors
K. L. Tanaka, D.A. Senske, M. Price, Randolph L. Kirk
Index to detailed maps of landslides in the San Francisco Bay region, California Index to detailed maps of landslides in the San Francisco Bay region, California
No abstract available.
Authors
Richard J. Pike
Options for the Future of the US National Strong-Motion Program Options for the Future of the US National Strong-Motion Program
This report constitutes the requested 'Options Document'. This report considers three options. Option I assumes a constant level of financial support for Operating Expenses (OE) with not additional personnel support. Option II assumes a slight increase in OE support of $150K for FY 99 and beyond. Option III considers the role that a NSMP must play if the nation's urgent need to record...
Authors
Hydraulic modeling of unsteady debris-flow surges with solid-fluid interactions Hydraulic modeling of unsteady debris-flow surges with solid-fluid interactions
Interactions of solid and fluid constituents produce the unique style of motion that typifies debris flows. To simulate this motion, a new hydraulic model represents debris flows as deforming masses of granular solids variably liquefied by viscous pore fluid. The momentum equation of the model describes how internal and boundary forces change as coarse-grained surge heads dominated by...
Authors
Richard M. Iverson