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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

The history of late holocene surface-faulting earthquakes on the central segments of the Wasatch fault zone, Utah The history of late holocene surface-faulting earthquakes on the central segments of the Wasatch fault zone, Utah

The Wasatch fault (WFZ)—Utah’s longest and most active normal fault—forms a prominent eastern boundary to the Basin and Range Province in northern Utah. To provide paleoseismic data for a Wasatch Front regional earthquake forecast, we synthesized paleoseismic data to define the timing and displacements of late Holocene surface-faulting earthquakes on the central five segments of the WFZ...
Authors
Christopher DuRoss, Stephen Personius, Susan S Olig, Anthony J. Crone, Michael D. Hylland, William R. Lund, David P. Schwartz

A 600-year-long stratigraphic record of tsunamis in south-central Chile 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...
Authors
Isabel Hong, Tina Dura, Lisa L. Ely, Benajamin P. Horton, Alan R. Nelson, Marco Cisternas, Daria Nikitina, Robert L. Wesson

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

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

Imaging of earthquake faults using small UAVs as a pathfinder for air and space observations Imaging of earthquake faults using small UAVs as a pathfinder for air and space observations

Large earthquakes cause billions of dollars in damage and extensive loss of life and property. Geodetic and topographic imaging provide measurements of transient and long-term crustal deformation needed to monitor fault zones and understand earthquakes. Earthquake-induced strain and rupture characteristics are expressed in topographic features imprinted on the landscapes of fault zones...
Authors
Andrea Donnellan, Joseph Green, Adnan Ansar, Joseph Aletky, Margaret Glasscoe, Yehuda Ben-Zion, J. Ramon Arrowsmith, Stephen B. DeLong

Amplification of earthquake ground motions in Washington, DC, and implications for hazard assessments in central and eastern North America 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...
Authors
Thomas L. Pratt, J. Wright Horton, Jessica Munoz, Susan E. Hough, Martin C. Chapman, C. Guney Olgun

The HayWired Earthquake Scenario The HayWired Earthquake Scenario

Foreword The 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...

Control of landslide volume and hazard by glacial stratigraphic architecture, Northwest Washington state, USA Control of landslide volume and hazard by glacial stratigraphic architecture, Northwest Washington state, USA

Landslide volumes span many orders of magnitude, but large-volume slides tend to travel farther and consequently can pose a greater hazard. In northwest Washington State, USA, a landscape abounding with landslides big and small, the recent occurrence of the large-volume and tragically deadly State Route 530 (Oso) landslide is a stark reminder of the hazards associated with glacial...
Authors
Jonathan Perkins, Mark E. Reid, Kevin M. Schmidt

Extreme geomagnetic storms: Probabilistic forecasts and their uncertainties Extreme geomagnetic storms: Probabilistic forecasts and their uncertainties

Extreme space weather events are low-frequency, high-risk phenomena. Estimating their rates of occurrence, as well as their associated uncertainties, is difficult. In this study, we derive statistical estimates and uncertainties for the occurrence rate of an extreme geomagnetic storm on the scale of the Carrington event (or worse) occurring within the next decade. We model the...
Authors
Pete Riley, Jeffrey J. Love
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