Publications
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Landslide deposit boundaries for the Little North Santiam River Basin, Oregon Landslide deposit boundaries for the Little North Santiam River Basin, Oregon
This layer is an inventory of existing landslides deposits in the Little North Santiam River Basin, Oregon (2009). Each landslide deposit shown on this map has been classified according to a number of specific characteristics identified at the time recorded in the GIS database. The classification scheme was developed by the Oregon Department of Geology and Mineral Industries (Burns and...
Authors
Steven Sobieszczyk
An empirical model for global earthquake fatality estimation An empirical model for global earthquake fatality estimation
We analyzed mortality rates of earthquakes worldwide and developed a country/region-specific empirical model for earthquake fatality estimation within the U.S. Geological Survey's Prompt Assessment of Global Earthquakes for Response (PAGER) system. The earthquake fatality rate is defined as total killed divided by total population exposed at specific shaking intensity level. The total...
Authors
Kishor Jaiswal, David Wald
Location of photographs showing landslide features in the Little North Santiam River Basin, Oregon Location of photographs showing landslide features in the Little North Santiam River Basin, Oregon
Data points represent locations of photographs taken of landslides in the Little North Santiam River Basin, Oregon. Photos were taken in spring of 2010 during field verification of landslide locations (deposits previously mapped using LiDAR-derived imagery). The photographs depict various landslide features, such as scarps, pistol-butt trees, or colluvium deposits. This work was...
Authors
Steven Sobieszczyk
Landslide inventory for the Little North Santiam River Basin, Oregon Landslide inventory for the Little North Santiam River Basin, Oregon
This geodatabase is an inventory of existing landslides in the Little North Santiam River Basin, Oregon (2009). Each landslide feature shown has been classified according to a number of specific characteristics identified at the time recorded in the GIS database. The classification scheme was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009)...
Authors
Steven Sobieszczyk
Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan
A typhoon (Typhoon No. 10) attacked Shikoku Island and the Tyugoku area of Japan in 2004. This typhoon produced a new daily precipitation record of 1317 mm on Shikoku Island and triggered hundreds of landslides in Tokushima Prefecture. One catastrophic landslide was triggered in the Shiraishi area of Kisawa village, and destroyed more than 10 houses while also leaving an unstable block...
Authors
G. Wang, A. Suemine, W.H. Schulz
High tsunami frequency as a result of combined strike-slip faulting and coastal landslides High tsunami frequency as a result of combined strike-slip faulting and coastal landslides
Earthquakes on strike-slip faults can produce devastating natural hazards. However, because they consist predominantly of lateral motion, these faults are rarely associated with significant uplift or tsunami generation. And although submarine slides can generate tsunami, only a few per cent of all tsunami are believed to be triggered in this way. The 12 January Mw 7.0 Haiti earthquake...
Authors
Matthew J. Hornbach, Nicole Braudy, Richard W. Briggs, Marie-Helene Cormier, Marcy B. Davis, John B. Diebold, Nicole Dieudonne, Roby Douilly, Cliff Frohlich, Sean P.S. Gulick, Harold E. Johnson, Paul Mann, Cecilia McHugh, Katherine Ryan-Mishkin, Carol S. Prentice, Leonardo Seeber, Christopher C. Sorlien, Michael S. Steckler, Steeve Julien Symithe, Frederick W. Taylor, John Templeton
Global earthquake casualties due to secondary effects: A quantitative analysis for improving PAGER losses Global earthquake casualties due to secondary effects: A quantitative analysis for improving PAGER losses
This study presents a quantitative and geospatial description of global losses due to earthquake-induced secondary effects, including landslide, liquefaction, tsunami, and fire for events during the past 40 years. These processes are of great importance to the US Geological Survey’s (USGS) Prompt Assessment of Global Earthquakes for Response (PAGER) system, which is currently being...
Authors
Kristin Marano, David J. Wald, Trevor Allen
Tree-ring dated landslide movements and seismic events in southwestern Montana, USA Tree-ring dated landslide movements and seismic events in southwestern Montana, USA
Because many tree species can live for several centuries or longer (Brown 1996), tree-ring analysis can be a valuable tool to date geomorphic events such as landslides, earthquakes, and avalanches in regions lacking long historical records. Typically, a catastrophic landslide will destroy all trees on the landslide, but trees on slower moving landslides may survive. For example, the...
Authors
Paul E. Carrara, J. Michael O’Neill
Top of head scarp and internal scarps for landslide deposits in the Little North Santiam River Basin, Oregon Top of head scarp and internal scarps for landslide deposits in the Little North Santiam River Basin, Oregon
Data points represent head scarps, flank scarps, and minor internal scarps (linear) associated with landslide deposits in the Little North Santiam River Basin, Oregon. This work was completed as part of the Master's thesis "Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009...
Authors
Steven Sobieszczyk
Analysis of elevation changes detected from multi-temporal LiDAR surveys in forested landslide terrain in western Oregon Analysis of elevation changes detected from multi-temporal LiDAR surveys in forested landslide terrain in western Oregon
We examined elevation changes detected from two successive sets of Light Detection and Ranging (LiDAR) data in the northern Coast Range of Oregon. The first set of LiDAR data was acquired during leafon conditions and the second set during leaf-off conditions. We were able to successfully identify and map active landslides using a differential digital elevation model (DEM) created from...
Authors
W.J. Burns, J. A. Coe, B.S. Kaya, Liwang Ma
The GSN and large earthquakes The GSN and large earthquakes
No abstract available.
Authors
Gavin P. Hayes, Hiroo Kanamori, Thorne Lay, Charles J. Ammon
Predicting the probability and volume of postwildfire debris flows in the intermountain western United States Predicting the probability and volume of postwildfire debris flows in the intermountain western United States
Empirical models to estimate the probability of occurrence and volume of postwildfire debris flows can be quickly implemented in a geographic information system (GIS) to generate debris-flow hazard maps either before or immediately following wildfires. Models that can be used to calculate the probability of debris-flow production from individual drainage basins in response to a given...
Authors
S.H. Cannon, J.E. Gartner, M.G. Rupert, J. A. Michael, A. H. Rea, C. Parrett