Publications
Filter Total Items: 7576
Ambient field seismology in critical zone hydrological sciences Ambient field seismology in critical zone hydrological sciences
Passive ambient noise monitoring is an emerging tool in environmental seismology, leveraging the ambient seismic field to assess temporal variations in shallow subsurface properties. This review focuses on the potential and challenges of using scattered coda waves from noise correlation functions to monitor critical zone dynamics. The sensitivity of seismic velocities to various...
Authors
Marine A. Denolle, Qibin Shi, Timothy Hugh Clements, Loic Viens, Veronica Rodriguez-Tribaldos, Fabrice Cotton
Earthquake magnitude and source parameter estimation with a distributed acoustic sensing dataset in the Gorda subduction zone Earthquake magnitude and source parameter estimation with a distributed acoustic sensing dataset in the Gorda subduction zone
Distributed acoustic sensing (DAS) systems offer a cost‐effective way to create large‐scale strainmeter arrays for seismological applications using fiber‐optic cables. DAS‐based strain measurements are known to be influenced by various factors, bringing into question their general reliability for accurate earthquake characterization. A 15‐km‐long DAS deployment in northern California was
Authors
Andrew J. Barbour, Jeffrey J. McGuire, Martin Karrenbach, Robert McPherson, Mark Hemphill-Haley, Connie Stewart
ShakeAlert®—Communication, education, outreach and technical engagement strategic vision ShakeAlert®—Communication, education, outreach and technical engagement strategic vision
Executive Summary In 2006, the U.S. Geological Survey (USGS) began directly supporting ShakeAlert® research and in 2012 the ShakeAlert demonstration system began testing (Given and others, 2018). The ShakeAlert earthquake early warning (EEW) system is a partnership between the U.S. Geological Survey (USGS) and the three West Coast States (Washington, Oregon, and California) served by the
Authors
Robert Michael deGroot, Sara K. McBride, Margaret J. Vinci, Gabriel C. Lotto, Megan L. Anderson, Danielle F. Sumy, Brian Terbush
Three-dimensional seismic velocity model for the Cascadia Subduction Zone with shallow soils and topography, version 1.7 Three-dimensional seismic velocity model for the Cascadia Subduction Zone with shallow soils and topography, version 1.7
The U.S. Geological Survey’s seismic velocity model for the Cascadia Subduction Zone provides P- and S-wave velocity (VP and VS, respectively) information from 40.2° to 50.0° N. latitude and −129.0° to −121.0° W. longitude, and is used to support a variety of research topics, including three-dimensional (3D) earthquake simulations and seismic hazard assessment in the Pacific Northwest...
Authors
Erin A. Wirth, Alex R. Grant, Ian P. Stone, William J. Stephenson, Arthur D. Frankel
Earthquake probabilities and hazards in the U.S. Pacific Northwest Earthquake probabilities and hazards in the U.S. Pacific Northwest
Earthquakes and their cascading consequences pose a significant threat to the people, environment, infrastructure, and economy of the U.S. Pacific Northwest. The Pacific Northwest is susceptible to three types of earthquakes: deep (intraslab) earthquakes, subduction zone (megathrust) earthquakes, and shallow crustal earthquakes. For each of these earthquake types, earth scientists can...
Authors
Erin A. Wirth, Arthur D. Frankel, Brian L. Sherrod, Alex R. Grant, Audrey Dunham, Ian P. Stone, Julia Grossman
To heal or not to heal?: 2. The moment-recurrence time behavior of repeating earthquakes in the 2011 Prague, Oklahoma aftershock sequence is consistent with laboratory healing rates To heal or not to heal?: 2. The moment-recurrence time behavior of repeating earthquakes in the 2011 Prague, Oklahoma aftershock sequence is consistent with laboratory healing rates
The timing and failure conditions of an earthquake are governed by the interplay between fault reloading and restrengthening. The moment-recurrence time behavior of repeating earthquakes can give observational estimates of fault healing rates; however, it is difficult to link these observed healing rates to laboratory studies of frictional healing in part because of uncertainty in...
Authors
Kristina Okamoto, Heather M. Savage, Elizabeth S. Cochran, Emily Brodsky, Rachel E. Abercrombie
A soil velocity model for improved ground motion simulations in the U. S. Pacific Northwest A soil velocity model for improved ground motion simulations in the U. S. Pacific Northwest
Near-surface seismic velocity structure may significantly impact the intensity, duration, and frequency content of ground shaking during an earthquake. In this study, we compile 649 shear wave velocity (Vs) profiles throughout the U.S. Pacific Northwest and southern British Columbia (PNW) and use these measured profiles to develop a representative soil velocity model for four major...
Authors
Alex R. Grant, Erin A. Wirth, Ian P. Stone
Mechanics and statistics of postseismic shaking Mechanics and statistics of postseismic shaking
Analysis of two weeks of continuous post-seismic shaking after the 2019 M7.1 Ridgecrest, CA earthquake sequence using 4 nearby borehole seismometers reveals that continuous ground motions decay as Omori’s law in time and follow the Gutenberg-Richter distribution in logarithmic amplitude. The measured temporal decay in amplitudes agrees with predictions of the rate-and-state framework and...
Authors
Timothy Hugh Clements, Elizabeth S. Cochran, Sarah E. Minson, Nicholas van der Elst, Clara Yoon, Annemarie S. Baltay, Morgan T. Page
Did they feel it? Legacy maroseismic data illuminates an engimatic 20th century earthquake Did they feel it? Legacy maroseismic data illuminates an engimatic 20th century earthquake
The challenges and the importance of preserving legacy instrumental records of earthquakes are now well-recognized (e.g., Richards & Hellweg, 2020, https://doi.org/10.1785/0220200053). Seismologists may not be aware of parallel challenges and opportunities with legacy macroseismic data for earthquakes in the United States. For much of the 20th century, macroseismic data were collected by...
Authors
Susan E. Hough, Lori Dengler, Robert McPherson, Lijam Hagos, Margaret Hellweg
Seismic response of rock towers at the Trona Pinnacles (U.S.A.) to the 2019 Ridgecrest earthquake sequence: Theory, observations, and models Seismic response of rock towers at the Trona Pinnacles (U.S.A.) to the 2019 Ridgecrest earthquake sequence: Theory, observations, and models
We analyze the seismic response of a class of fragile geologic features (FGFs), referred to as rock towers (RTs) at the Trona Pinnacles, a group of RTs in southern California that suffered strong shaking during the 2019 Ridgecrest earthquake sequence. FGFs, including RTs, may provide maximum constraints on past earthquake shaking intensity, and thereby support probabilistic seismic...
Authors
Joaquin Garcia Suarez, Devin McPhillips, Domniki Asimaki
Induced earthquakes are generally not tidally triggered in Oklahoma and Kansas Induced earthquakes are generally not tidally triggered in Oklahoma and Kansas
Human-induced earthquakes occur along critically stressed faults as injected wastewater simultaneously heightens fluid pressure and pushes faults to failure. We investigate the possibility that small stresses imposed by Earth tides could trigger earthquakes in the induced seismicity region of Oklahoma and Kansas from 2011 to 2018. We decluster a catalog consisting of ∼110,000 earthquakes...
Authors
Margaret Elizabeth Glasgow, Justin L. Rubinstein, Jeanne L. Hardebeck
Python Hyperspectral Analysis Tool (PyHAT) user guide Python Hyperspectral Analysis Tool (PyHAT) user guide
This report is a user guide for the 0.1.2 release of the Python Hyperspectral Analysis Tool (PyHAT) and its graphical user interface (GUI). The GUI is intended to provide an intuitive front end to allow users to apply sophisticated preprocessing and analysis methods to spectroscopic data. Though the PyHAT package has been developed with a particular focus on laser-induced breakdown...
Authors
Ryan B. Anderson, Itiya P. Aneece, Travis S.J. Gabriel