Publications
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Landslides across the United States: Occurrence, susceptibility, and data limitations Landslides across the United States: Occurrence, susceptibility, and data limitations
Detailed information about landslide occurrence is the foundation for advancing process understanding, susceptibility mapping, and risk reduction. Despite the recent revolution in digital elevation data and remote sensing technologies, landslide mapping remains resource intensive. Consequently, a modern, comprehensive map of landslide occurrence across the United States (USA) has not...
Authors
Benjamin B. Mirus, Eric S. Jones, Rex L. Baum, Jonathan W. Godt, Stephen L. Slaughter, Matthew Crawford, Jeremy T. Lancaster, Thomas Stanley, Dalia Kirschbaum, William J. Burns, Robert G. Schmitt, Kassandra O Lindsey, Kevin McCoy
Observations of coastal change and numerical modeling of sediment-transport pathways at the mouth of the Columbia River and its adjacent littoral cell Observations of coastal change and numerical modeling of sediment-transport pathways at the mouth of the Columbia River and its adjacent littoral cell
Bathymetric and topographic surveys performed annually along the coastlines of northern Oregon and southwestern Washington documented changes in beach and nearshore morphology between 2014 and 2019. Volume change analysis revealed measurable localized erosion and deposition throughout the study area, but significant net erosion at the regional scale (several kilometers [km]) was limited...
Authors
Andrew W. Stevens, Edwin Elias, Stuart Pearson, George M. Kaminsky, Peter R Ruggiero, Heather M. Weiner, Guy R. Gelfenbaum
When source and path components trade off in ground-motion prediction equations When source and path components trade off in ground-motion prediction equations
Current research on ground‐motion models (also known as ground‐motion prediction equations [GMPEs]) and their uncertainties focus on the separate contributions of source, path, and site to both median values and their variability. Implicit here is the assumption that the event term, path term, and site term reflect only properties of the source, path, and site, respectively. Events with...
Authors
Annemarie S. Baltay Sundstrom, Lauren S. Abrahams, Thomas C. Hanks
Rapid geodetic observations of spatiotemporally varying postseismic deformation following the Ridgecrest earthquake sequence: The U.S. Geological Survey response Rapid geodetic observations of spatiotemporally varying postseismic deformation following the Ridgecrest earthquake sequence: The U.S. Geological Survey response
The U.S. Geological Survey’s geodetic response to the 4–5 July 2019 (Pacific time) Ridgecrest earthquake sequence comprised primarily the installation and/or reoccupation of Global Navigation Satellite System (GNSS) monumentation. Our response focused primarily on the United States’ Navy’s China Lake Naval Air Weapons Station base (NAWSCL). This focus was because much of the surface...
Authors
Benjamin A. Brooks, Jessica R. Murray, Jerry L. Svarc, Ellen L. Phillips, Ryan Clayton Turner, Mark Hunter Murray, Todd Ericksen, Kang Wang, Sarah E. Minson, Roland Burgmann, Frederick Pollitz, Kenneth W. Hudnut, Johanna Nevitt, Evelyn Roeloffs, Janis Hernandez, Brian Olson
Minimal clustering of injection-induced earthquakes observed with a large-n seismic array Minimal clustering of injection-induced earthquakes observed with a large-n seismic array
The clustering behavior of injection‐induced earthquakes is examined using one month of data recorded by the LArge‐n Seismic Survey in Oklahoma (LASSO) array. The 1829‐node seismic array was deployed in a 25 km×32 km area of active saltwater disposal in northern Oklahoma between 14 April and 10 May 2016. Injection rates in the study area are nearly constant around the time of the...
Authors
Elizabeth S. Cochran, A. Wickham-Piotrowski, K. Kemna, R. M Harrington, S. Dougherty, A. Pena Castro
Impacts of sea-level rise on the tidal reach of California coastal rivers using the Coastal Storm Modeling System (CoSMoS) Impacts of sea-level rise on the tidal reach of California coastal rivers using the Coastal Storm Modeling System (CoSMoS)
In coastal rivers, the interactions between tides and fluvial discharge affect local ecology, sedimentation, river dynamics, river mouth configuration, and the flooding potential in adjacent wetlands and low-lying areas. With sea-level rise, the tidal reach within coastal rivers can expand upstream, impacting river dynamics and increasing flood risk across a much greater area. Rivers...
Authors
Andrea C. O'Neill, Li H. Erikson, Patrick L. Barnard
Peak ground velocity spatial variability revealed by dense seismic array in southern California Peak ground velocity spatial variability revealed by dense seismic array in southern California
Understanding and modeling variability of ground motion is essential for building accurate and precise ground motion prediction equations, which can net site‐specific characterization and reduced hazard levels. Here, we explore the spatial variability in peak ground velocity (PGV) at Sage Brush Flats along the San Jacinto Fault in southern California. We use data from a dense array (0.6...
Authors
Christopher E Johnson, Debi Kilb, Annemarie S. Baltay Sundstrom, Frank Vernon
Hydro-morphological characterization of coral reefs for wave runup prediction Hydro-morphological characterization of coral reefs for wave runup prediction
Many coral reef-lined coasts are low-lying with elevations 30,000) dataset of measured coral reef topobathymetric cross-shore profiles, statistics, machine learning, and numerical modeling to develop a set of representative cluster profiles (RCPs) that can be used to accurately represent the shoreline hydrodynamics of a large variety of coral reef-lined coasts around the globe. In two...
Authors
Fred Scott, Jose A.A. Antolinez, Robert T. McCall, Curt D. Storlazzi, Ad Reiners, Stuart Pearson
Submarine canyons, slope failures and mass transport processes in southern Cascadia Submarine canyons, slope failures and mass transport processes in southern Cascadia
The marine turbidite record along the southern Cascadia Subduction Zone has been used to interpret paleoseismicity and suggest a shorter recurrence interval for large (>M7) earthquakes along this portion of the margin; however, the sources and pathways of these turbidity flows are poorly constrained. We examine the spatial distribution of sediment storage, downslope transport, and slope...
Authors
Jenna C. Hill, Janet Watt, Daniel S. Brothers, Jared W. Kluesner
Mild displacements of boulders during the 2019 Ridgecrest Earthquakes Mild displacements of boulders during the 2019 Ridgecrest Earthquakes
Strong seismic waves from the July 2019 Ridgecrest, California, earthquakes displaced rocks in proximity to the M 7.1 mainshock fault trace at several locations. In this report, we document large boulders that were displaced at the Wagon Wheel Staging Area (WWSA), approximately 4.5 km southeast of the southern terminus of the large M 6.4 foreshock rupture (hereafter “the large foreshock”...
Authors
Norman Sleep, Susan E. Hough
Ten ways Mount St. Helens changed our world—The enduring legacy of the 1980 eruption Ten ways Mount St. Helens changed our world—The enduring legacy of the 1980 eruption
Mount St. Helens was once enjoyed for its serene beauty and was considered one of America’s most majestic volcanoes because of its perfect cone shape, similar to Japan’s beloved Mount Fuji. Nearby residents assumed that the mountain was solid and enduring. That perception changed during the early spring of 1980. Then, on May 18, 1980, following 2 months of earthquakes and small...
Authors
Carolyn L. Driedger, Jon J. Major, John S. Pallister, Michael A. Clynne, Seth C. Moran, Elizabeth G. Westby, John W. Ewert
Late Quaternary slip rates on the Sierra Madre fault zone and paleoseismic evidence on the size and frequency of past ruptures Late Quaternary slip rates on the Sierra Madre fault zone and paleoseismic evidence on the size and frequency of past ruptures
The Sierra Madre fault zone is a south-vergent, active reverse fault that accommodates shortening between basins on the northern margin of the Los Angeles region and the San Gabriel Mountains. The preservation of late Quaternary alluvial fill and fan surfaces in the hanging wall of the fault provides evidence of long-term uplift. Surface rupture from the 1971 Mw 6.6 San Fernando...
Authors
Reed J. Burgette, Katherine M. Scharer, Scott Lindvall