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Interaction of dams and landslides: Case studies and mitigation Interaction of dams and landslides: Case studies and mitigation

In the first half of the 20th century, engineering geology and geotechnical engineering were in their infancy, and dams were often built where landslides provided valley constrictions, often without expert site investigation. Only the most important projects were subjected to careful geologic examination. Thus, dams were often built without complete understanding of the possible...
Authors
Robert L. Schuster

Post-Wildfire Sedimentation in Saguaro National Park, Rincon Mountain District, and Effects on Lowland Leopard Frog Habitat Post-Wildfire Sedimentation in Saguaro National Park, Rincon Mountain District, and Effects on Lowland Leopard Frog Habitat

The Rincon Mountain District of Saguaro National Park occupies about 272 square kilometers of mountains, canyons, and alluvial fans in southeastern Arizona just east of Tucson. The park contains some of the last remaining habitat in the Tucson Basin of the lowland leopard frog that lives in the bedrock pools called tinajas in canyons at elevations between 850 and 1,800 meters. Those...
Authors
John T.C. Parker

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 W. 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 L. Harp, John A. Michael, William T. 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 F. Chleborad, Rex L. Baum, Jonathan W. 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 L. Harp, Anthony J. 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 M. 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 E. Reid, Dianne Brien

A plastic flow model for the Acquara - Vadoncello landslide in Senerchia, Southern Italy A plastic flow model for the Acquara - Vadoncello landslide in Senerchia, Southern Italy

A previously developed model for stress and velocity fields in two-dimensional Coulomb plastic materials under self-weight and pore pressure predicts that long, shallow landslides develop slip surfaces that manifest themselves as normal faults and normal fault scarps at the surface in areas of extending flow and as thrust faults and thrust fault scarps at the surface in areas of...
Authors
W. Savage, J. Wasowski

Varieties of submarine failure morphologies of seismically-induced landslides in Alaskan fjords Varieties of submarine failure morphologies of seismically-induced landslides in Alaskan fjords

The Great Alaska Earthquake of 1964 caused major damage and 43 deaths in the coastal communities of Seward and Valdez. Most of these losses were caused by tsunamis that occurred immediately after the earthquake and were most likely induced by local submarine landslides. Recent NOAA multibcam bathymetric surveys near Seward and Valdez provide detailed information about the morphology of...
Authors
H. Lee, H. Ryan, R. E. Kayen, Peter J. Haeussler, P. Dartnell, M. A. Hampton
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