Publications
Filter Total Items: 2186
Analysis of the origin of landslides in the New Madrid seismic zone
No abstract available.
Authors
R. W. Jibson, D. K. Keefer
Rapid water-level fluctuations in a thin colluvium landslide west of Cincinnati, Ohio
No abstract available.
Authors
William C. Haneberg, A. Onder Gokce
Preliminary geomagnetic paleointensities from Long Valley Caldera, California
Paleointensities are being determined in order to characterize geomagnetic intensity variations during Quaternary time. Because the geomagnetic field acts as a shield against cosmic radiation, its intensity directly affects the production rate of radiocarbon (^C) in the upper atmosphere. Coe and others (1978) showed that the variation in dipole moment during Holocene time is nearly proportional to
Authors
Edward A. Mankinen
Giant Hawaiian underwater landslides
No abstract available
Authors
James G. Moore, William R. Normark, Robin T. Holcomb
Giant Hawaiian landslides
Sixty-eight landslides more than 20 km long are present along a 2200 km segment of the Hawaiian Ridge from near Midway to Hawaii. Some of the landslides exceed 200 km in length and 5000 km3 in volume, ranking them among the largest on Earth. Most of these giant landslides were discovered during a mapping program of the U.S. Hawaiian Exclusive Economic zone from 1986 to 1991 utilizing the GLORIA si
Authors
J. G. Moore, W. R. Normark, R. T. Holcomb
A pore-pressure diffusion model for estimating landslide-inducing rainfall
Many types of landslide movement are induced by large rainstorms, and empirical rainfall intensity/duration thresholds for initiating movement have been determined for various parts of the world. In this paper, I present a simple pressure diffusion model that provides a physically based hydrologic link between rainfall intensity/duration at the ground surface and destabilizing pore-water pressures
Authors
M.E. Reid
The importance of earthquake-induced landslides to long-term slope erosion and slope-failure hazards in seismically active regions
This paper describes a general method for determining the amount of earthquake-induced landsliding that occurs in a seismically active region over time; this determination can be used as a quantitative measure of the long-term hazard from seismically triggered landslides as well as a measure of the importance of this process to regional slope-erosion rates and landscape evolution. The method uses
Authors
D. K. Keefer
Potential for seepage erosion of landslide dam
The failure potential of the debris-avalanche dam at Castle Lake near Mount St. Helens, Washington, by three processes of seepage erosion (1) Heave; (2) piping; and (3) internal erosion, is examined. Results indicated that the dam is stable against piping but potentially locally unstable against heave. -from Authors
Authors
W. Meyer, R. L. Schuster, M. A. Sabol
Modeling and analysis of the 1949 Narrows landslide, Tacoma, Washington
A large landslide failed catastrophically along steep, 90-m (300-ft) high bluffs overlooking the waters of Puget Sound at Tacoma, Washington, in April of 1949, three days after the region was struck by a magnitude 7.1 earthquake. The area of failure was investigated to estimate the static and seismic stability of the pre-earthquake slope and to identify factors that contributed to the failure. Res
Authors
A.F. Chleborad
Landslides triggered by the Northridge earthquake
No abstract available.
Authors
R. W. Jibson, E. L. Harp, D. K. Keefer, R. C. Wilson