Publications
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Characteristics, extent and origin of hydrothermal alteration at Mount Rainier Volcano, Cascades Arc, USA: Implications for debris-flow hazards and mineral deposits Characteristics, extent and origin of hydrothermal alteration at Mount Rainier Volcano, Cascades Arc, USA: Implications for debris-flow hazards and mineral deposits
Hydrothermal alteration at Mount Rainier waxed and waned over the 500,000-year episodic growth of the edifice. Hydrothermal minerals and their stable-isotope compositions in samples collected from outcrop and as clasts from Holocene debris-flow deposits identify three distinct hypogene argillic/advanced argillic hydrothermal environments: magmatic-hydrothermal, steam-heated, and magmatic...
Authors
D. A. John, T. W. Sisson, G. N. Breit, R. O. Rye, J.W. Vallance
Modeling rainfall conditions for shallow landsliding in Seattle, Washington Modeling rainfall conditions for shallow landsliding in Seattle, Washington
We describe the results from an application of a distributed, transient infiltration–slope-stability model for an 18 km2 area of southwestern Seattle, Washington, USA. The model (TRIGRS) combines an infinite slope-stability calculation and an analytic, one-dimensional solution for pore-pressure diffusion in a soil layer of finite depth in response to time-varying rainfall. The transient...
Authors
Jonathan W. Godt, William H. Schulz, Rex L. Baum, William Z. Savage
The USGS Caribbean Seismic Network The USGS Caribbean Seismic Network
Jamaica, Cuba, Turks and Caicos, Domincan Republic, Antigua-Barbuda, Grenada, Barbados, Panama, Honduras—what an itinerary! Palm trees, beaches, iguanas and seismic stations.
Authors
Lind Gee, Dan McNamara, Jean Weaver, Harley Benz, Doug Ford, Gay Gyure
Modeling the spatial distribution of landslide-prone colluvium and shallow groundwater on hillslopes of Seattle, WA Modeling the spatial distribution of landslide-prone colluvium and shallow groundwater on hillslopes of Seattle, WA
Landslides in partially saturated colluvium on Seattle, WA, hillslopes have resulted in property damage and human casualties. We developed statistical models of colluvium and shallow-groundwater distributions to aid landslide hazard assessments. The models were developed using a geographic information system, digital geologic maps, digital topography, subsurface exploration results, the
Authors
W.H. Schulz, D. J. Lidke, J. W. Godt
Documentation for the 2008 update of the United States National Seismic Hazard Maps Documentation for the 2008 update of the United States National Seismic Hazard Maps
The 2008 U.S. Geological Survey (USGS) National Seismic Hazard Maps display earthquake ground motions for various probability levels across the United States and are applied in seismic provisions of building codes, insurance rate structures, risk assessments, and other public policy. This update of the maps incorporates new findings on earthquake ground shaking, faults, seismicity, and...
Authors
Mark D. Petersen, Arthur D. Frankel, Stephen C. Harmsen, Charles S. Mueller, Kathleen M. Haller, Russell L. Wheeler, Robert L. Wesson, Yuehua Zeng, Oliver S. Boyd, David M. Perkins, Nicolas Luco, Edward H. Field, Chris J. Wills, Kenneth S. Rukstales
Landslides triggered by the 8 October 2005 Kashmir earthquake Landslides triggered by the 8 October 2005 Kashmir earthquake
The 8 October 2005 Kashmir earthquake triggered several thousand landslides. These were mainly rock falls and debris falls, although translational rock and debris slides also occurred. In addition, a sturzstrom (debris avalanche) comprising ??? 80??million m3 buried four villages and blocked streams to create two lakes. Although landsliding occurred throughout the region, covering an...
Authors
L.A. Owen, U. Kamp, G.A. Khattak, E. L. Harp, D. K. Keefer, M.A. Bauer
Post-wildfire erosion response in two geologic terrains in the western USA Post-wildfire erosion response in two geologic terrains in the western USA
Volumes of eroded sediment after wildfires vary substantially throughout different geologic terrains across the western United States. These volumes are difficult to compare because they represent the response to rainstorms and runoff with different characteristics. However, by measuring the erosion response as the erodibility efficiency of water to detach and transport sediment on...
Authors
J. A. Moody, D.A. Martin, S.H. Cannon
Landslide risk in the San Francisco Bay region Landslide risk in the San Francisco Bay region
We have used historical records of damaging landslides triggered by rainstorms, and a newly developed Probabilistic Landslide Assessment Cost Estimation System (PLACES), to estimate the numbers and direct costs of future landslides in the San Francisco Bay region. The estimated annual cost of future landslides in the entire region is about US $15 million (year 2000 $). The estimated...
Authors
J. A. Coe, R. A. Crovelli
Development of hazard-compatible building fragility and vulnerability models Development of hazard-compatible building fragility and vulnerability models
We present a methodology for transforming the structural and non-structural fragility functions in HAZUS into a format that is compatible with conventional seismic hazard analysis information. The methodology makes use of the building capacity (or pushover) curves and related building parameters provided in HAZUS. Instead of the capacity spectrum method applied in HAZUS, building...
Authors
E. Karaca, N. Luco
Landslides and engineering geology of the Seattle, Washington, area Landslides and engineering geology of the Seattle, Washington, area
This volume brings together case studies and summary papers describing the application of state-of-the-art engineering geologic methods to landslide hazard analysis for the Seattle, Washington, area. An introductory chapter provides a thorough description of the Quaternary and bedrock geology of Seattle. Nine additional chapters review the history of landslide mapping in Seattle, present...
Authors
Rex L. Baum, Jonathan W. Godt, Lynn M. Highland
Converting HAZUS capacity curves to seismic hazard-compatible building fragility functions: effect of hysteretic models Converting HAZUS capacity curves to seismic hazard-compatible building fragility functions: effect of hysteretic models
A methodology was recently proposed for the development of hazard-compatible building fragility models using parameters of capacity curves and damage state thresholds from HAZUS (Karaca and Luco, 2008). In the methodology, HAZUS curvilinear capacity curves were used to define nonlinear dynamic SDOF models that were subjected to the nonlinear time history analysis instead of the capacity...
Authors
Hyeuk Ryu, Nicolas Luco, Jack W. Baker, Erdem Karaca
Rapid Assessment of earthquake-induced landsliding Rapid Assessment of earthquake-induced landsliding
The Pacific Northwest in the United States including Seattle, Washington, experienced unusually heavy rainfall in the winters of 1995/1996 and 1996/1997, which caused numerous landslides. Following these two winters, the City of Seattle resolved to reduce future landslide losses within its jurisdiction. By coincidence, in 1997 the U.S. Geological Survey (USGS) began a five-year project...
Authors
J. W. Godt, B. Sener, K.L. Verdin, D.J. Wald, P.S. Earle, E. L. Harp, R.W. Jibson