Publications
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Investigating landslides caused by earthquakes - A historical review Investigating landslides caused by earthquakes - A historical review
Post-earthquake field investigations of landslide occurrence have provided a basis for understanding, evaluating, and mapping the hazard and risk associated with earthquake-induced landslides. This paper traces the historical development of knowledge derived from these investigations. Before 1783, historical accounts of the occurrence of landslides in earthquake are typically so...
Authors
D. K. Keefer
Shallow seismic imaging of folds above the Puente Hills blind-thrust fault, Los Angeles, California Shallow seismic imaging of folds above the Puente Hills blind-thrust fault, Los Angeles, California
High-resolution seismic reflection profiles image discrete folds in the shallow subsurface (
Authors
Thomas L. Pratt, John H. Shaw, James F. Dolan, Shari A. Christofferson, Robert Williams, Jack K. Odum, Andreas Plesch
The proximal part of the giant submarine Wailau landslide, Molokai, Hawaii The proximal part of the giant submarine Wailau landslide, Molokai, Hawaii
The main break-in-slope on the northern submarine flank of Molokai at -1500 to -1250 m is a shoreline feature that has been only modestly modified by the Wailau landslide. Submarine canyons above the break-in-slope, including one meandering stream, were subaerially carved. Where such canyons cross the break-in-slope, plunge pools may form by erosion from bedload sediment carried down the...
Authors
D.A. Clague, J.G. Moore
Magnetic fields over active tectonic zones in ocean Magnetic fields over active tectonic zones in ocean
The aim of our work is to estimate the electromagnetic effects that can be detected in the submarine zones with hydrothermal activity. It is known that meso-scale flows appear in the regions over underwater volcanoes or hot rocks. Their origin is connected with heat flux and hot jets released from underwater volcanoes or faults in a sea bottom. Values of mean velocities and turbulent...
Authors
Yu. A. Kopytenko, P.M. Serebrianaya, L.V. Nikitina, A.W. Green
Geomorphic studies of landslides in the Tully Valley, New York: Implications for public policy and planning Geomorphic studies of landslides in the Tully Valley, New York: Implications for public policy and planning
On April 27, 1993, a large landslide in the Tully Valley, Onondaga County, NY, destroyed three houses and resulted in the evacuation of four others; it also triggered a loss of potable drinking water for about 15 homes north of the slide area and affected a total of 20 ha of land. In the 7 years following this slide, several studies have been conducted by federal and state environmental...
Authors
D. L. Pair, William M. Kappel
Comparing landslide inventories: The map depends on the method Comparing landslide inventories: The map depends on the method
Landslide inventory maps are generally prepared by interpreting the geomorphic expression of landsliding on aerial photos, topographic maps, or on the ground. Distinctive landslide geomorphology allows the recognition and mapping of landslides, although there are always landslides that have very subtle expression and are not identified. The difficulties of mapping landslides based on...
Authors
C.J. Wills, T.P. McCrink
Landslide susceptibility map of Tegucigalpa, Honduras Landslide susceptibility map of Tegucigalpa, Honduras
No abstract available.
Authors
Edwin L. Harp
Identifying a large landslide with small displacements in a zone of coseismic tectonic deformation; the Villa Del Monte landslide triggered by the 1989 Loma Prieta, California, earthquake Identifying a large landslide with small displacements in a zone of coseismic tectonic deformation; the Villa Del Monte landslide triggered by the 1989 Loma Prieta, California, earthquake
The Villa Del Monte landslide was one of 20 large and complex landslides triggered by the 1989 LomaPrieta, California, earthquake in a zone of pervasive coseismicground cracking near the fault rupture. The landslide was approximately 980 m long, 870 m wide, and encompassed an area of approximately 68 ha. Drilling data suggested that movement may have extended to depths as great as 85 m...
Authors
David K. Keefer, Edwin L. Harp, Gary B. Griggs, Stephen G. Evans, Jerome V. DeGraff
Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event
40Ar/39Ar ages were determined on the three major ash-flow tuffs of the Yellowstone Plateau volcanic field in the region of Yellowstone National Park in order to improve the precision of previously determined ages. Total-fusion and incremental- heating ages of sanidine yielded the following mean ages: Huckleberry Ridge Tuff—2.059 ± 0.004 Ma; Mesa Falls Tuff— 1.285 ± 0.004 Ma; and Lava...
Authors
M. A. Lanphere, D.E. Champion, R.L. Christiansen, G. A. Izett, J. D. Obradovich
Stability assessment of a Hurricane Mitch-induced landslide dam on the Rio La Lima, Sierra de Las Minas, eastern Guatemala Stability assessment of a Hurricane Mitch-induced landslide dam on the Rio La Lima, Sierra de Las Minas, eastern Guatemala
No abstract available.
Authors
Robert L. Schuster, Robert C. Bucknam, Manuel Antonio Mota
Socioeconomic and environmental impacts of landslides in the Western Hemisphere Socioeconomic and environmental impacts of landslides in the Western Hemisphere
In spite of improvements in recognition, prediction, mitigative measures, and warning systems, economic losses and casualties due to landslides in the Western Hemisphere appear to be growing as a result of increasing development of landslide-prone areas due to population pressures. This paper notes outstanding examples of socioeconomic losses in the Americas. Landslides impact the...
Authors
Robert L. Schuster, Lynn M. Highland
Observations and recommendations regarding landslide hazards related to the January 13, 2001 M-7.6 El Salvador earthquake Observations and recommendations regarding landslide hazards related to the January 13, 2001 M-7.6 El Salvador earthquake
The January 13, 2001 earthquake (M-7.6) off the coast of El Salvador triggered widespread damaging landslides in many parts of the El Salvador. In the aftermath of the earthquake, the Salvadoran government requested technical assistance through the U.S. Agency for International Development (USAID); USAID, in turn, requested help from technical experts in landslide hazards from the U.S...
Authors
Randall W. Jibson, Anthony J. Crone