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Site response, shallow shear-wave velocity, and wave propagation at the San Jose, California, dense seismic array Site response, shallow shear-wave velocity, and wave propagation at the San Jose, California, dense seismic array

Ground-motion records from a 52-element dense seismic array near San Jose, California, are analyzed to obtain site response, shallow shear-wave velocity, and plane-wave propagation characteristics. The array, located on the eastern side of the Santa Clara Valley south of the San Francisco Bay, is sited over the Evergreen basin, a 7-km-deep depression with Miocene and younger deposits...
Authors
S. Hartzell, D. Carver, R. A. Williams, S. Harmsen, A. Zerva

Using multiple logistic regression and GIS technology to predict landslide hazard in northeast Kansas, USA Using multiple logistic regression and GIS technology to predict landslide hazard in northeast Kansas, USA

Landslides in the hilly terrain along the Kansas and Missouri rivers in northeastern Kansas have caused millions of dollars in property damage during the last decade. To address this problem, a statistical method called multiple logistic regression has been used to create a landslide-hazard map for Atchison, Kansas, and surrounding areas. Data included digitized geology, slopes, and...
Authors
G.C. Ohlmacher, J.C. Davis

Tree-ring dated landslide movements and their relationship to seismic events in southwestern Montana, USA Tree-ring dated landslide movements and their relationship to seismic events in southwestern Montana, USA

To determine periods of incremental landslide movement and their possible relationship to regional seismic events, the tree-ring records of 32 titled and damaged conifers at three sites on landslides in the Gravelly Range of southwestern Montana were examined. Several signs of disturbance in the tree-ring record indicating landslide movement were observed. Commonly, the tree-ring record...
Authors
Paul E. Carrara, J.M. O’Neill

Debris-flow hazards caused by hydrologic events at Mount Rainier, Washington Debris-flow hazards caused by hydrologic events at Mount Rainier, Washington

At 4393 m, ice-clad Mount Rainier has great potential for debris flows owing to its precipitous slopes and incised steep valleys, the large volume of water stored in its glaciers, and a mantle of loose debris on its slopes. In the past 10,000 years, more than sixty Holocene lahars have occurred at Mount Rainier (Scott et al., 1985), and, in addition more than thirty debris flows not...
Authors
James W. Vallance, Michelle L. Cunico, Steve P. Schilling

Gaussian statistics for palaeomagnetic vectors Gaussian statistics for palaeomagnetic vectors

With the aim of treating the statistics of palaeomagnetic directions and intensities jointly and consistently, we represent the mean and the variance of palaeomagnetic vectors, at a particular site and of a particular polarity, by a probability density function in a Cartesian three-space of orthogonal magnetic-field components consisting of a single (unimoda) non-zero mean, spherically...
Authors
Jeffrey J. Love, C.G. Constable

Emergency assessment of potential debris-flow peak discharges, Coal Seam fire, Colorado Emergency assessment of potential debris-flow peak discharges, Coal Seam fire, Colorado

These maps present the results of assessments of peak discharges that can potentially be generated by debris flows issuing from the basins burned by the Coal Seam fire of June and July 2002, near Glenwood Springs, Colorado. The maps are based on a regression model for debris-flow peak discharge normalized by average storm intensity as a function of basin gradient and burned extent, and...
Authors
Susan H. Cannon, John A. Michael, Joseph E. Gartner, Alan H. Rea, Steven P. Garcia

Interpreting the earthquake source of the Wabash Valley seismic zone (Illinois, Indiana, and Kentucky) from seismic-reflection, gravity, and magnetic-intensity data Interpreting the earthquake source of the Wabash Valley seismic zone (Illinois, Indiana, and Kentucky) from seismic-reflection, gravity, and magnetic-intensity data

Reprocessing of seismic-reflection data reveals new images of upper- to middle-crustal structures beneath the Wabash Valley seismic zone, located north of the New Madrid seismic zone within the seismically active southern Illinois basin. Four intersecting deep seismic profiles (243 km total) indicate an anomalous, 5–10-km-wide zone of dipping reflections and diffractions below the...
Authors
John H. McBride, Thomas G. Hildenbrand, William J. Stephenson, Christopher J. Potter

Emergency assessment of potential debris-flow peak discharges, Missionary Ridge fire, Colorado Emergency assessment of potential debris-flow peak discharges, Missionary Ridge fire, Colorado

These maps present the results of assessments of peak discharges that can potentially be generated by debris flows issuing from the basins burned by the Missionary Ridge fire of June 9 through July 14, 2002, near Durango, Colorado. The maps are based on a regression model for debris-flow peak discharge normalized by average storm intensity as a function of basin gradient and burned...
Authors
Susan H. Cannon, Alan H. Rea, J. Andrew Gleason, Stephen P. Garcia

Natural hazards on alluvial fans: The Venezuela debris flow and flash flood disaster Natural hazards on alluvial fans: The Venezuela debris flow and flash flood disaster

In December 1999, rainstorms induced thousands of landslides along the Cordillera de la Costa, Vargas, northern Venezuela. Rainfall on December 2-3 totaled 200 millimeters (8 inches) and was followed by a major storm (911 millimeters, or 36 inches) on December 14 through 16. Debris flows and flash floods on alluvial fans inundated coastal communities, caused severe property destruction...
Authors
Matthew C. Larsen, Gerald F. Wieczoreck, L. Scott Eaton, Benjamin A. Morgan, Heriberto Torres-Sierra

Digital inventory of landslides and related deposits in Honduras triggered by Hurricane Mitch Digital inventory of landslides and related deposits in Honduras triggered by Hurricane Mitch

Intense rainfall from Hurricane Mitch from October 27-31, 1998, exceeded 900 mm in places in Honduras and triggered in excess of 500,000 landslides throughout the country. Landslides damaged an estimated 70% of the road network in Honduras based on estimates by the U. S Army Corps of Engineers. Numbers of fatalities due to landslides are not accurately known due to the fact that numerous...
Authors
Edwin L. Harp, Kirk W. Hagaman, Matthew D. Held, Jonathan P. McKenna
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