Publications
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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
Isolated cases of remote dynamic triggering in Canada detected using cataloged earthquakes combined with a matched-filter approach Isolated cases of remote dynamic triggering in Canada detected using cataloged earthquakes combined with a matched-filter approach
Here we search for dynamically triggered earthquakes in Canada following global main shocks between 2004 and 2014 with MS > 6, depth 0.2 cm/s. We use the Natural Resources Canada (NRCan) earthquake catalog to calculate β statistical values in 1° × 1° bins in 10 day windows before and after the main shocks. The statistical analysis suggests that triggering may occur near Vancouver Island...
Authors
Wang Bei, Rebecca M. Harrington, Yajing Liu, Hongyu Yu, Alex Carey, Nicholas van der Elst
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
Overview The primary mission of the U.S. Geological Survey (USGS) National Earthquake Information Center (NEIC) is comprehensive global earthquake monitoring (M4.5 or larger) and complete seismic monitoring of the United States for all significant earthquakes (M3.0 or larger or felt). In recent years, the NEIC has assumed a more prominent role in local and regional seismic monitoring...
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 importance of dunes on a variety of planetary surfaces The importance of dunes on a variety of planetary surfaces
Scientists observe aeolian bed forms, or dune-like structures, throughout the solar system in a range of locations, from bodies with only transient atmospheres, such as comets, to places with thick atmospheres, such as Venus and the Earth’s ocean floor. Determining the source of sand and the different dune formations that result are thus important to understanding solar system and...
Authors
Timothy N. Titus, James R. Zimbelman, Jani Radebaugh
Collections management plan for the U.S. Geological Survey Woods Hole Coastal and Marine Science Center Data Library Collections management plan for the U.S. Geological Survey Woods Hole Coastal and Marine Science Center Data Library
The U.S. Geological Survey Woods Hole Coastal and Marine Science Center has created a Data Library to organize, preserve, and make available the field, laboratory, and modeling data collected and processed by Woods Hole Coastal and Marine Science Center staff. This Data Library supports current research efforts by providing unique, historic datasets with accompanying metadata. The Woods...
Authors
Kelleen M. List, Brian J. Buczkowski, Linda P. McCarthy, Alice M. Orton
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
Strong ground motion inferred from liquefaction caused by the 1811-1812 New Madrid, Missouri, earthquakes Strong ground motion inferred from liquefaction caused by the 1811-1812 New Madrid, Missouri, earthquakes
Peak ground accelerations (PGAs) in the epicentral region of the 1811–1812 New Madrid, Missouri, earthquakes are inferred from liquefaction to have been no greater than ∼0.35g. PGA is inferred in an 11,380 km2 area in the Lower Mississippi Valley in Arkansas and Missouri where liquefaction was extensive in 1811–1812. PGA was inferred by applying liquefaction probability curves, which...
Authors
Thomas L. Holzer, Thomas E. Noce, Michael J. Bennett
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
Earthquake forewarning in the Cascadia region Earthquake forewarning in the Cascadia region
This report, prepared for the National Earthquake Prediction Evaluation Council (NEPEC), is intended as a step toward improving communications about earthquake hazards between information providers and users who coordinate emergency-response activities in the Cascadia region of the Pacific Northwest. NEPEC charged a subcommittee of scientists with writing this report about forewarnings...
Authors
Joan S. Gomberg, Brian F. Atwater, Nicholas M. Beeler, Paul Bodin, Earl Davis, Arthur D. Frankel, Gavin P. Hayes, Laura McConnell, Tim Melbourne, David H. Oppenheimer, John G. Parrish, Evelyn A. Roeloffs, Gary D. Rogers, Brian L. Sherrod, John Vidale, Timothy J. Walsh, Craig S. Weaver, Paul M. Whitmore
Estimating rates of debris flow entrainment from ground vibrations Estimating rates of debris flow entrainment from ground vibrations
Debris flows generate seismic waves as they travel downslope and can become more dangerous as they entrain sediment along their path. We present field observations that show a systematic relation between the magnitude of seismic waves and the amount of erodible sediment beneath the flow. Specifically, we observe that a debris flow traveling along a channel filled initially with sediment...
Authors
Jason W. Kean, Jeffrey A. Coe, V. Coviello, Joel B. Smith, S.W. McCoy, M. Arattano
California State Waters Map Series — Offshore of Bodega Head, California California State Waters Map Series — Offshore of Bodega Head, California
Introduction In 2007, the California Ocean Protection Council initiated the California Seafloor Mapping Program (CSMP), designed to create a comprehensive seafloor map of high-resolution bathymetry, marine benthic habitats, and geology within the 3-nautical-mile limit of California’s State Waters. The CSMP approach is to create highly detailed seafloor maps through collection...
Authors
Samuel Y. Johnson, Peter Dartnell, Nadine E. Golden, Stephen R. Hartwell, Mercedes D. Erdey, H. Gary Greene, Guy R. Cochrane, Rikk G. Kvitek, Michael W. Manson, Charles A. Endris, Bryan E. Dieter, Janet Watt, Lisa M. Krigsman, Ray W. Sliter, Erik N. Lowe, John L. Chin