Publications
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Landslides and megathrust splay faults captured by the late Holocene sediment record of eastern Prince William Sound, Alaska Landslides and megathrust splay faults captured by the late Holocene sediment record of eastern Prince William Sound, Alaska
We present new marine seismic‐reflection profiles and bathymetric maps to characterize Holocene depositional patterns, submarine landslides, and active faults beneath eastern and central Prince William Sound (PWS), Alaska, which is the eastern rupture patch of the 1964 Mw 9.2 earthquake. We show evidence that submarine landslides, many of which are likely earthquake triggered, repeatedly...
Authors
S.P. Finn, Lee M. Liberty, Peter J. Haeussler, Thomas L. Pratt
Seismicity of the Earth 1900‒2013 Mediterranean Sea and vicinity Seismicity of the Earth 1900‒2013 Mediterranean Sea and vicinity
The Mediterranean region is seismically active due to the convergence of the Africa Plate with the Eurasia plate. Present day Africa-Eurasia motion ranges from ~4 millimeters per year (mm/yr) in a northwest-southeast direction in the western Mediterranean to ~10 mm/yr (north-south) in the eastern Mediterranean. The Africa-Eurasia plate boundary is complex, and includes extensional and
Authors
Matthew W. Herman, Gavin P. Hayes, Gregory M. Smoczyk, Rebecca Turner, Bethan Turner, Jennifer Jenkins, Sian Davies, Amy Parker, Allison Sinclair, Harley M. Benz, Kevin P. Furlong, Antonio Villaseñor
Ground motion simulation for the 23 August 2011, Mineral, Virginia earthquake using physics-based and stochastic broadband methods Ground motion simulation for the 23 August 2011, Mineral, Virginia earthquake using physics-based and stochastic broadband methods
Three broadband simulation methods are used to generate synthetic ground motions for the 2011 Mineral, Virginia, earthquake and compare with observed motions. The methods include a physics‐based model by Hartzell et al. (1999, 2005), a stochastic source‐based model by Boore (2009), and a stochastic site‐based model by Rezaeian and Der Kiureghian (2010, 2012). The ground‐motion dataset...
Authors
Xiaodan Sun, Stephen H. Hartzell, Sanaz Rezaeian
Estimating annualized earthquake losses for the conterminous United States Estimating annualized earthquake losses for the conterminous United States
We make use of the most recent National Seismic Hazard Maps (the years 2008 and 2014 cycles), updated census data on population, and economic exposure estimates of general building stock to quantify annualized earthquake loss (AEL) for the conterminous United States. The AEL analyses were performed using the Federal Emergency Management Agency's (FEMA) Hazus software, which facilitated a
Authors
Kishor S. Jaiswal, Douglas Bausch, Rui Chen, Jawhar Bouabid, Hope Seligson
Upgrade of the New China Digital Seismograph Network Upgrade of the New China Digital Seismograph Network
No abstract available.
Authors
D. Anderson, J. Anderson, D. Ford, Lind S. Gee, G. Gyure, Charles R. Hutt, E. Kromer, B. Marshall, K. Persefield, Adam T. Ringler, M. Sharratt, Tyler Storm, David C. Wilson, D. Yang, Z. Zheng
Observatory geoelectric fields induced in a two-layer lithosphere during magnetic storms Observatory geoelectric fields induced in a two-layer lithosphere during magnetic storms
We report on the development and validation of an algorithm for estimating geoelectric fields induced in the lithosphere beneath an observatory during a magnetic storm. To accommodate induction in three-dimensional lithospheric electrical conductivity, we analyze a simple nine-parameter model: two horizontal layers, each with uniform electrical conductivity properties given by...
Authors
Jeffrey J. Love, Andrei Swidinsky
Plugs or flood-makers? the unstable landslide dams of eastern Oregon Plugs or flood-makers? the unstable landslide dams of eastern Oregon
Landslides into valley bottoms can affect longitudinal profiles of rivers, thereby influencing landscape evolution through base-level changes. Large landslides can hinder river incision by temporarily damming rivers, but catastrophic failure of landslide dams may generate large floods that could promote incision. Dam stability therefore strongly modulates the effects of landslide dams...
Authors
Elizabeth B. Safran, Jim E. O'Connor, Lisa L. Ely, Kyle House, Gordon E. Grant, Kelsey Harrity, Kelsey Croall, Emily Jones
By
Geology, Energy, and Minerals Mission Area, Natural Hazards Mission Area, Energy Resources Program, Groundwater and Streamflow Information Program, Landslide Hazards Program, Mineral Resources Program, Science and Decisions Center, Volcano Hazards Program, Volcano Science Center, Geologic Hazards Science Center, Geology, Minerals, Energy, and Geophysics Science Center
On- and off-fault deformation associated with the September 2013 Mw7.7 Balochistan earthquake: Implications for geologic slip rate measurements On- and off-fault deformation associated with the September 2013 Mw7.7 Balochistan earthquake: Implications for geologic slip rate measurements
The 24 September 2013 Mw7.7 Balochistan, Pakistan earthquake ruptured a ~ 200 km-long stretch of the Hoshab fault in southern Pakistan and produced the second-largest lateral surface displacement observed for a continental strike-slip earthquake. We remotely measured surface deformation associated with this event using high-resolution (0.5 m) pre- and post-event satellite optical imagery...
Authors
Ryan D. Gold, Nadine G. Reitman, Richard W. Briggs, William D. Barnhart, Gavin P. Hayes, Earl M. Wilson
A rapid estimation of near field tsunami run-up A rapid estimation of near field tsunami run-up
Many efforts have been made to quickly estimate the maximum run-up height of tsunamis associated with large earthquakes. This is a difficult task, because of the time it takes to construct a tsunami model using real time data from the source. It is possible to construct a database of potential seismic sources and their corresponding tsunami a priori.However, such models are generally...
Authors
Sebastian Riqueime, Mauricio Fuentes, Gavin P. Hayes, Jamie Campos
National Earthquake Information Center systems overview and integration National Earthquake Information Center systems overview and integration
Authors
Michelle R. Guy, John M. Patton, Jeremy Fee, Mike Hearne, Eric Martinez, D. Ketchum, Charles Worden, Vince Quitoriano, Edward Hunter, Gregory Smoczyk, Stan Schwarz
The Boulder magnetic observatory The Boulder magnetic observatory
The Boulder magnetic observatory has, since 1963, been operated by the Geomagnetism Program of the U.S. Geological Survey in accordance with Bureau and national priorities. Data from the observatory are used for a wide variety of scientific purposes, both pure and applied. The observatory also supports developmental projects within the Geomagnetism Program and collaborative projects with...
Authors
Jeffrey J. Love, Carol A. Finn, Kolby L. Pedrie, Cletus C. Blum
Earthquake shaking hazard estimates and exposure changes in the conterminous United States Earthquake shaking hazard estimates and exposure changes in the conterminous United States
A large portion of the population of the United States lives in areas vulnerable to earthquake hazards. This investigation aims to quantify population and infrastructure exposure within the conterminous U.S. that are subjected to varying levels of earthquake ground motions by systematically analyzing the last four cycles of the U.S. Geological Survey's (USGS) National Seismic Hazard...
Authors
Kishor S. Jaiswal, Mark D. Petersen, Kenneth S. Rukstales, William S. Leith