Publications
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Mid-Continent Geographic Science Center Natural Hazards Research - Landslides Mid-Continent Geographic Science Center Natural Hazards Research - Landslides
No abstract available.
Authors
Water Resources Division U.S. Geological Survey
Photographs, correspondence, and presentations related to the La Conchita, California, landslide Photographs, correspondence, and presentations related to the La Conchita, California, landslide
This report contains the following photographs and information related to the La Conchita, California, landslide: 1) Digital photographs taken by the author during a visit to the La Conchita landslide on January 14, 2005. 2) Correspondence related to the approval and release of USGS Open-File Report 2005-1067, Landslide Hazards at La Conchita, California. 3) A presentation on the La...
Authors
Randall Jibson
Shallow-landslide hazard map of Seattle, Washington Shallow-landslide hazard map of Seattle, Washington
Landslides, particularly debris flows, have long been a significant cause of damage and destruction to people and property in the Puget Sound region. Following the years of 1996 and 1997, the Federal Emergency Management Agency (FEMA) designated Seattle as a 'Project Impact' city with the goal of encouraging the city to become more disaster resistant to the effects of landslides and...
Authors
Edwin Harp, John Michael, William Laprade
Rainfall thresholds for forecasting landslides in the Seattle, Washington, area — Exceedance and probability Rainfall thresholds for forecasting landslides in the Seattle, Washington, area — Exceedance and probability
Empirical rainfall thresholds and related information form a basis for forecasting landslides in the Seattle area. A formula for a cumulative rainfall threshold (CT), P3=3.5–0.67P15, defined by rainfall amounts (in inches) during the last 3 days (72 hours), P3, and the previous 15 days (360 hours), P15, was developed from analysis of historical data for 91 landslides that occurred as...
Authors
Alan Chleborad, Rex Baum, Jonathan Godt
Landslides triggered by the October 8, 2005, Pakistan earthquake and associated landslide-dammed reservoirs Landslides triggered by the October 8, 2005, Pakistan earthquake and associated landslide-dammed reservoirs
The October 8, 2005, Kashmir earthquake (M 7.6) triggered several thousand landslides, mainly rock falls and rock slides, in the epicentral area near the cities of Muzafarrabad and Balakot, Pakistan. Most of these were shallow, coalescing rock slides emanating from highly sheared and deformed limestone and dolomite of the Precambrian Muzafarrabad Formation. The largest landslide...
Authors
Edwin Harp, Anthony Crone
Estimating landslide losses - preliminary results of a seven-State pilot project Estimating landslide losses - preliminary results of a seven-State pilot project
Introduction: In 2001, the U.S. Geological Survey Landslide Hazards Program provided funding for seven State geological surveys to report on the status of landslide investigation strategies in each of their States, and to suggest improved ways to approach the tracking of landslides, their effects, losses associated with the landslides, and hazard mitigation strategies. Each State was to...
Authors
Lynn Highland
Assessing massive flank collapse at stratovolcanoes using 3-D slope stability analysis Assessing massive flank collapse at stratovolcanoes using 3-D slope stability analysis
Massive rock failures pose one of the greatest hazards at stratovolcanoes; more than 20,000 fatalities have resulted worldwide from historical volcano edifice collapses. Although numerous processes can destabilize an edifice, gravitational instability is strongly influenced by the interplay of topography, variable potential failure surfaces, and the three-dimensional (3-D) distributions...
Authors
Mark Reid, Dianne Brien
Landslides triggered by the 2004 Niigata Ken Chuetsu, Japan, earthquake Landslides triggered by the 2004 Niigata Ken Chuetsu, Japan, earthquake
The Niigata Ken Chuetsu earthquake triggered a vast number of lanslides in the epicentral region. Landslide concentrations were among the highest ever measured after an earthquake, and most of the triggered landslides were relatively shallow failures parallel to the steep slope faces. The dense concentration of landslides can be attributed to steep local topography in relatively weak...
Authors
D.S. Kieffer, R. Jibson, E.M. Rathje, K. Kelson
The 2005 La Conchita, California, landslide The 2005 La Conchita, California, landslide
[No abstract available]
Authors
R.W. Jibson
Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico
We have established for the first time a size frequency distribution for carbonate submarine slope failures. Using detailed bathymetry along the northern edge of the carbonate platform north of Puerto Rico, we show that the cumulative distribution of slope failure volumes follows a power-law distribution. The power-law exponent of this distribution is similar to those for rock falls on...
Authors
Uri S. ten Brink, E.L. Geist, B.D. Andrews
Two models for evaluating landslide hazards Two models for evaluating landslide hazards
Two alternative procedures for estimating landslide hazards were evaluated using data on topographic digital elevation models (DEMs) and bedrock lithologies in an area adjacent to the Missouri River in Atchison County, Kansas, USA. The two procedures are based on the likelihood ratio model but utilize different assumptions. The empirical likelihood ratio model is based on non-parametric...
Authors
J.C. Davis, C.-J. Chung, G.C. Ohlmacher