Publications
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Earthquake information products and tools from the Advanced National Seismic System (ANSS) Earthquake information products and tools from the Advanced National Seismic System (ANSS)
This Fact Sheet provides a brief description of postearthquake tools and products provided by the Advanced National Seismic System (ANSS) through the U.S. Geological Survey Earthquake Hazards Program. The focus is on products specifically aimed at providing situational awareness in the period immediately following significant earthquake events.
Authors
Lisa Wald
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
An overview of the global variability in radiated energy and apparent stress An overview of the global variability in radiated energy and apparent stress
a global study of radiated seismic energies ER and apparent stresses τ a reveals systematic patterns. earthquakes with the highest apparent stress occur in regions of intense deformation and rupture strong lithosphere. in oceanic settings, these are strike-slip earthquakes (τ a up to 27 Mpa) occurring intraplate or at evolving ends of transform faults. at subduction zones and...
Authors
George Choy, Arthur McGarr, Stephen Kirby, John Boatwright
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
Statistical modeling of storm-level Kp occurrences Statistical modeling of storm-level Kp occurrences
We consider the statistical modeling of the occurrence in time of large Kp magnetic storms as a Poisson process, testing whether or not relatively rare, large Kp events can be considered to arise from a stochastic, sequential, and memoryless process. For a Poisson process, the wait times between successive events occur statistically with an exponential density function. Fitting an...
Authors
K.J. Remick, Jeffrey Love
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
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. Kayen, Peter Haeussler, P. Dartnell, M. Hampton
Do migratory flight paths of raptors follow constant geographical or geomagnetic courses? Do migratory flight paths of raptors follow constant geographical or geomagnetic courses?
We tested whether routes of raptors migrating over areas with homogeneous topography follow constant geomagnetic courses more or less closely than constant geographical courses. We analysed the routes taken over land of 45 individual raptors tracked by satellite-based radiotelemetry: 25 peregrine falcons, Falco peregrinus, on autumn migration between North and South America, and seven...
Authors
K. Thorup, M. Fuller, T. Alerstam, M. Hake, N. Kjellen, R. Strandberg
Landslides caused by the M 7.6 Tecomán, Mexico earthquake of January 21, 2003 Landslides caused by the M 7.6 Tecomán, Mexico earthquake of January 21, 2003
The Tecomán, Mexico earthquake (also called the “Colima earthquake”) of January 21, 2003 (M 7.6) triggered several hundreds of landslides in the coastal cordilleras of Colima State, near the earthquake source, and several thousands in the volcanic highlands north and northwest of Colima City. These landslides, mostly shallow and disrupted failures, caused minor damage to roads, to a...
Authors
David Keefer, Joseph Wartman, Ochoa Navarro, Adrian Rodriguez-Marek, Gerald Wieczorek