Publications
Filter Total Items: 7620
Oklahoma experiences largest earthquake during ongoing regional wastewater injection hazard mitigation efforts 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...
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 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...
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 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...
Authors
Mehmet Celebi, J. Hooper, Ron Klemencic
Effects of lava heating on volatile-rich slopes on Io Effects of lava heating on volatile-rich slopes on Io
The upper crust of Io may be very rich in volatile sulfur and SO2. The surface is also highly volcanically active, and slopes may be warmed by radiant heat from the lava. This is particularly the case in paterae, which commonly host volcanic eruptions and long-lived lava lakes. Paterae slopes are highly variable, but some are greater than 70°. I model the heating of a volatile slope for...
Authors
Colin M. Dundas
Granular flows at recurring slope lineae on Mars indicate a limited role for liquid water Granular flows at recurring slope lineae on Mars indicate a limited role for liquid water
Recent liquid water flow on Mars has been proposed based on geomorphological features, such as gullies. Recurring slope lineae — seasonal flows that are darker than their surroundings — are candidate locations for seeping liquid water on Mars today, but their formation mechanism remains unclear. Topographical analysis shows that the terminal slopes of recurring slope lineae match the...
Authors
Colin M. Dundas, Alfred S. McEwen, Matthew Chojnacki, Moses P. Milazzo, Shane Byrne, Jim McElwaine, Anna Urso
Geologic overview of the Mars Science Laboratory rover mission at the Kimberley, Gale crater, Mars Geologic overview of the Mars Science Laboratory rover mission at the Kimberley, Gale crater, Mars
The Mars Science Laboratory (MSL) Curiosity rover completed a detailed investigation at the Kimberley waypoint within Gale crater from sols 571-634 using its full science instrument payload. From orbital images examined early in the Curiosity mission, the Kimberley region had been identified as a high-priority science target based on its clear stratigraphic relationships in a layered...
Authors
Melissa Rice, Sanjeev Gupta, Allan H. Treiman, Kathryn M. Stack, Fred J. Calef, Lauren A. Edgar, John P. Grotzinger, Nina L. Lanza, Laetitia Le Deit, Jeremie Lasue, Kirsten L. Siebach, Ashwin R. Vasavada, Roger C. Wiens, Josh Williams
Investigation of input reduction techniques for morphodynamic modeling of complex inlets with baroclinic forcing Investigation of input reduction techniques for morphodynamic modeling of complex inlets with baroclinic forcing
The Mouth of the Columbia River (MCR) is a complex estuary inlet system characterized by a buoyant plume created by high freshwater flows from the Columbia River into the Pacific Ocean. Data obtained during two major field campaigns have resulted in a comprehensive dataset of hydrodynamics and sediment transport under high (2013) and low (2005) river flow conditions. Through the analysis...
Authors
Guy R. Gelfenbaum, Edwin Elias, Andrew W. Stevens
Effects of topographic data quality on estimates of shallow slope stability using different regolith depth models Effects of topographic data quality on estimates of shallow slope stability using different regolith depth models
Thickness of colluvium or regolith overlying bedrock or other consolidated materials is a major factor in determining stability of unconsolidated earth materials on steep slopes. Many efforts to model spatially distributed slope stability, for example to assess susceptibility to shallow landslides, have relied on estimates of constant thickness, constant depth, or simple models of...
Authors
Rex L. Baum
Thumbnail‐based questionnaires for the rapid and efficient collection of macroseismic data from global earthquakes 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...
Authors
Remy Bossu, Matthieu Landes, Frederic Roussel, Robert Steed, Gilles Mazet-Roux, Stacey S. Martin, Susan E. Hough
Reexamination of the magnitudes for the 1906 and 1922 Chilean earthquakes using Japanese tsunami amplitudes: Implications for source depth constraints Reexamination of the magnitudes for the 1906 and 1922 Chilean earthquakes using Japanese tsunami amplitudes: Implications for source depth constraints
Far-field tsunami records from the Japanese tide gauge network allow the reexamination of the moment magnitudes (Mw) for the 1906 and 1922 Chilean earthquakes, which to date rely on limited information mainly from seismological observations alone. Tide gauges along the Japanese coast provide extensive records of tsunamis triggered by six great (Mw >8) Chilean earthquakes with...
Authors
M. Carvajal, M. Cisternas, A. Gubler, P. A. Catalan, P. Winckler, Robert L. Wesson
Geologic setting of the proposed West Flank Forge Site, California: Suitability for EGS research and development 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...
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
Micro-seismicity within the Coso Geothermal field, California, from 1996-2012 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...
Authors
J. Ole Kaven, Stephen H. Hickman, Lisa C. Weber