Publications
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A unified model of crustal stress heterogeneity from borehole breakouts and earthquake focal mechanisms A unified model of crustal stress heterogeneity from borehole breakouts and earthquake focal mechanisms
Observations of crustal stress orientation from the regional inversion of earthquake focal mechanisms often conflict with those from borehole breakouts, possibly indicating local stress heterogeneity, either laterally or with depth. To investigate this heterogeneity, we compiled SHmax estimates from previous studies for 57 near‐vertical boreholes with measured breakout azimuths across...
Authors
Karen Luttrell, Jeanne L. Hardebeck
Rupture process of the M6.5 Stanley, Idaho, earthquake inferred from seismic waveform and geodetic data Rupture process of the M6.5 Stanley, Idaho, earthquake inferred from seismic waveform and geodetic data
The 2020 M 6.5 Stanley, Idaho, earthquake produced rupture in the north of the active Sawtooth fault in the northern basin and range at depth, without any observable surface rupture. Global Positioning System (GPS) and Interferometric Synthetic Aperture Radar (InSAR) data yield several millimeters of static offsets out to ∼100 km from the rupture and up to ∼0.1 m of near‐field crustal
Authors
Frederick Pollitz, William C. Hammond, Charles Wicks
The impacts of the 2015/2016 El Niño on California's sandy beaches The impacts of the 2015/2016 El Niño on California's sandy beaches
The El Niño Southern Oscillation is the most dominant mode of interannual climate variability in the Pacific. The 2015/2016 El Niño event was one of the strongest of the last 145 years, resulting in anomalously high wave energy across the U.S. West Coast, and record coastal erosion for many California beaches. To better manage coastal resources, it is critical to understand the impacts...
Authors
Schuyler A Smith, Patrick L. Barnard
Rapid sensitivity analysis for reducing uncertainty in landslide hazard assessments Rapid sensitivity analysis for reducing uncertainty in landslide hazard assessments
One of the challenges in assessing temporal and spatial aspects of landslide hazard using process-based models is estimating model input parameters, especially in areas where limited measurements of soil and rock properties are available. In an effort to simplify and streamline parameter estimation, development of a simple, rapid approach to sensitivity analysis relies on field...
Authors
Rex L. Baum
On the use of statistical analysis to understand submarine landslide processes and assess their hazard On the use of statistical analysis to understand submarine landslide processes and assess their hazard
Because of their inaccessibility, submarine landslides are typically studied individually and at great effort and expense to provide knowledge of the specific site conditions where these landslides occur. Statistical analysis of submarine landslide scars can offer generalized perspectives on the processes that initiate submarine landslides and can help toward hazard assessment in areas...
Authors
Uri S. ten Brink, Eric L. Geist
Progress and lessons learned from responses to landslide disasters Progress and lessons learned from responses to landslide disasters
Landslides have the incredible power to transform landscapes and also, tragically, to cause disastrous societal impacts. Whereas the mechanics and effects of many landslide disasters have been analyzed in detail, the means by which landslide experts respond to these events has garnered much less attention. Herein, we evaluate nine landslide response case histories conducted by the U.S...
Authors
Brian D. Collins, Mark E. Reid, Jeffrey A. Coe, Jason W. Kean, Rex L. Baum, Randall W. Jibson, Jonathan W. Godt, Stephen Slaughter, Greg M. Stock
Spatial clustering of aftershocks impacts the performance of physics‐based earthquake forecasting models Spatial clustering of aftershocks impacts the performance of physics‐based earthquake forecasting models
I explore why physics‐based models of earthquake triggering rarely outperform statistical models in prospective testing, outside of limited spatial‐temporal windows. Pseudo‐prospective tests on suites of synthetic aftershock sequences show that a major factor is the level of unmodeled spatial clustering of the direct aftershocks triggered by the mainshock. The synthetic sequences are...
Authors
Jeanne L. Hardebeck
A long-term geothermal observatory across subseafloor gas hydrates, IODP Hole U1364A, Cascadia accretionary prism A long-term geothermal observatory across subseafloor gas hydrates, IODP Hole U1364A, Cascadia accretionary prism
We report 4 years of temperature profiles collected from May 2014 to May 2018 in Integrated Ocean Drilling Program Hole U1364A in the frontal accretionary prism of the Cascadia subduction zone. The temperature data extend to depths of nearly 300 m below seafloor (mbsf), spanning the gas hydrate stability zone at the location and a clear bottom-simulating reflector (BSR) at ∼230 mbsf...
Authors
K. Elizabeth Becker, E. E. Davis, M. Hessemann, J. A. Collins, Jeffrey J. McGuire
In‐situ mass balance estimates offshore Costa Rica In‐situ mass balance estimates offshore Costa Rica
The Costa Rican convergent margin has been considered a type erosive margin, with erosional models suggesting average losses up to −153 km3/km/m.y. However, three‐dimensional (3D) seismic reflection and Integrated Ocean Drilling Program data collected offshore the Osa Peninsula images accretionary structures and vertical motions that conflict with the forearc basal erosion model. Here we...
Authors
Joel Edwards, Jared W. Kluesner, Eli Silver, Rachel Lauer, Nathan Bangs, Brian Boston
The normal faulting 2020 Mw5.8 Lone Pine, Eastern California earthquake sequence The normal faulting 2020 Mw5.8 Lone Pine, Eastern California earthquake sequence
The 2020 Mw 5.8 Lone Pine earthquake, the largest earthquake on the Owens Valley fault zone, eastern California, since the nineteenth century, ruptured an extensional stepover in that fault. Owens Valley separates two normal‐faulting regimes, the western margin of the Great basin and the eastern margin of the Sierra Nevada, forming a complex seismotectonic zone, and a possible nascent...
Authors
Egill Hauksson, Brian J. Olsen, Alex R. Grant, Jennifer R Andrews, Angela I. Chung, Susan E. Hough, Hiroo Kanamori, Sara K. McBride, Andrew J. Michael, Morgan T. Page, Zachary E. Ross, Deborah Smith, Sotiris Valkaniotis
Numerical simulations of the geospace response to the arrival of an idealized perfect interplanetary coronal mass ejection Numerical simulations of the geospace response to the arrival of an idealized perfect interplanetary coronal mass ejection
Previously, Tsurutani and Lakhina (2014, https://doi.org/10.1002/2013GL058825) created estimates for a “perfect” interplanetary coronal mass ejection and performed simple calculations for the response of geospace, including . In this study, these estimates are used to drive a coupled magnetohydrodynamic-ring current-ionosphere model of geospace to obtain more physically accurate...
Authors
Daniel T. Welling, Jeffrey J. Love, E. Joshua Rigler, Denny M. Oliveira, Colin M. Komar, Steven Morley
Probabilistic application of an integrated catchment-estuary-coastal system model to assess the evolution of inlet-interrupted coasts over the 21st century Probabilistic application of an integrated catchment-estuary-coastal system model to assess the evolution of inlet-interrupted coasts over the 21st century
Inlet-interrupted sandy coasts are dynamic and complex coastal systems with continuously evolving geomorphological behaviors under the influences of both climate change and human activities. These coastal systems are of great importance to society (e.g., providing habitats, navigation, and recreational activities) and are affected by both oceanic and terrestrial processes. Therefore, the...
Authors
J. Bamunawala, Ali Dastgheib, Roshanka Ranasinghe, Ad van der Spek, Shreedhar Maskey, A. Brad Murray, Patrick L. Barnard, Trang Minh Duong, T.A.J.G. Sirisena