Publications
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Apparent late Quaternary fault slip rate increase in the southwestern Lower Rhine Graben, central Europe
In regions of low strain, long earthquake recurrence intervals (104–106 yrs) and erosive processes limit preservation of Quaternary markers suitable for distinguishing whether faults slip at uniform or secularly varying rates. The Lower Rhine graben in the border region of Germany, The Netherlands, and Belgium provides a unique opportunity to explore Quaternary slip‐rate variations in a region of
Authors
Ryan D. Gold, Anke M. Friedrich, Simon Kubler, Martin Salamon
Oklahoma experiences largest earthquake during ongoing regional wastewater injection hazard mitigation efforts
The 3 September 2016, Mw 5.8 Pawnee earthquake was the largest recorded earthquake in the state of Oklahoma. Seismic and geodetic observations of the Pawnee sequence, including precise hypocenter locations and moment tensor modeling, shows that the Pawnee earthquake occurred on a previously unknown left-lateral strike-slip basement fault that intersects the mapped right-lateral Labette fault zone.
Authors
William L. Yeck, Gavin P. Hayes, Daniel E. McNamara, Justin L. Rubinstein, William D. Barnhart, Paul S. Earle, Harley M. Benz
Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015
This paper describes the tectonic summaries for all magnitude 7 and larger earthquakes in the period 2000–2015, as produced by the U.S. Geological Survey National Earthquake Information Center during their routine response operations to global earthquakes. The goal of such summaries is to provide important event-specific information to the public rapidly and concisely, such that recent earthquakes
Authors
Gavin P. Hayes, Emma K. Meyers, James W. Dewey, Richard W. Briggs, Paul S. Earle, Harley M. Benz, Gregory M. Smoczyk, Hanna E. Flamme, William D. Barnhart, Ryan D. Gold, Kevin P. Furlong
Responses of a 64-story unique San Francisco, CA. building to four earthquakes and ambient motions
We analyze the ambient and earthquake responses of a 64-story, instrumented, concrete core shear wall building in San Francisco, Calif. equipped with tuned sloshing liquid dampers (TSDs) and buckling restraining braces (BRBs). In an earlier paper [1], only ambient data were used to identify dynamic characteristics. Recently, the 72-channel instrumental array of the building recorded the 24 August
Authors
Mehmet Çelebi, J. Hooper, Ron Klemencic
Micro-seismicity within the Coso Geothermal field, California, from 1996-2012
We extend our previous catalog of seismicity within the Coso Geothermal field by adding over two and a half years of additional data to prior results. In total, we locate over 16 years of seismicity spanning from April 1996 to May of 2012 using a refined velocity model, apply it to all events and utilize differential travel times in relocations to improve the accuracy of event locations. The impro
Authors
J. Ole Kaven, Stephen H. Hickman, Lisa C. Weber
Improvements in absolute seismometer sensitivity calibration using local earth gravity measurements
The ability to determine both absolute and relative seismic amplitudes is fundamentally limited by the accuracy and precision with which scientists are able to calibrate seismometer sensitivities and characterize their response. Currently, across the Global Seismic Network (GSN), errors in midband sensitivity exceed 3% at the 95% confidence interval and are the least‐constrained response parameter
Authors
Robert E. Anthony, Adam T. Ringler, David C. Wilson
The HayWired Earthquake Scenario
ForewordThe 1906 Great San Francisco earthquake (magnitude 7.8) and the 1989 Loma Prieta earthquake (magnitude 6.9) each motivated residents of the San Francisco Bay region to build countermeasures to earthquakes into the fabric of the region. Since Loma Prieta, bay-region communities, governments, and utilities have invested tens of billions of dollars in seismic upgrades and retrofits and replac
Amplification of earthquake ground motions in Washington, DC, and implications for hazard assessments in central and eastern North America
The extent of damage in Washington, DC, from the 2011 Mw 5.8 Mineral, VA, earthquake was surprising for an epicenter 130 km away; U.S. Geological Survey “Did-You-Feel-It” reports suggest that Atlantic Coastal Plain and other unconsolidated sediments amplified ground motions in the city. We measure this amplification relative to bedrock sites using earthquake signals recorded on a temporary seismom
Authors
Thomas L. Pratt, J. Wright Horton, Jessica Munoz, Susan E. Hough, Martin C. Chapman, C. Guney Olgun
A 600-year-long stratigraphic record of tsunamis in south-central Chile
The stratigraphy within coastal river valleys in south-central Chile clarifies and extends the region’s history of large, earthquakes and accompanying tsunamis. Our site at Quidico (38.1°S, 73.3°W) is located in an overlap zone between ruptures of magnitude 8–9 earthquakes in 1960 and 2010, and, therefore, records tsunamis originating from subduction-zone ruptures north and south of the city of Co
Authors
Isabel Hong, Tina Dura, Lisa L. Ely, Benajamin P. Horton, Alan R. Nelson, Marco Cisternas, Daria Nikitina, Robert L. Wesson
Implications of the earthquake cycle for inferring fault locking on the Cascadia megathrust
GPS velocity fields in the Western US have been interpreted with various physical models of the lithosphere-asthenosphere system: (1) time-independent block models; (2) time-dependent viscoelastic-cycle models, where deformation is driven by viscoelastic relaxation of the lower crust and upper mantle from past faulting events; (3) viscoelastic block models, a time-dependent variation of the block
Authors
Fred Pollitz, Eileen Evans
Geologic setting of the proposed West Flank Forge Site, California: Suitability for EGS research and development
The proposed West Flank FORGE site is within the China Lake Naval Air Weapons Station (NAWS), China Lake, CA. The West Flank is west of the Coso geothermal field, an area of China Lake NAWS dominated by the Quaternary Coso volcanic field largely comprised of rhyolite domes and their volcaniclastic and epiclastic horizons. The largest dome flow complex, Sugarloaf Mountain, marks the northwestern ma
Authors
Andrew Sabin, Kelly Blake, Mike Lazaro, Douglas Blankenship, Mack Kennedy, Jess McCullough, S.B. DeOreo, Stephen H. Hickman, Jonathan M.G. Glen, J. Ole Kaven, Colin F. Williams, Geoffrey Phelps, James E. Faulds, Nicholas H. Hinz, Wendy M. Calvin, Drew Siler, Ann Robertson-Tait
Thumbnail‐based questionnaires for the rapid and efficient collection of macroseismic data from global earthquakes
The collection of earthquake testimonies (i.e., qualitative descriptions of felt shaking) is essential for macroseismic studies (i.e., studies gathering information on how strongly an earthquake was felt in different places), and when done rapidly and systematically, improves situational awareness and in turn can contribute to efficient emergency response. In this study, we present advances made i
Authors
Remy Bossu, Matthieu Landes, Frederic Roussel, Robert Steed, Gilles Mazet-Roux, Stacey S. Martin, Susan E. Hough