Skip to main content
U.S. flag

An official website of the United States government

Publications

Filter Total Items: 7225

Crustal earthquake triggering by pre-historic great earthquakes on subduction zone thrusts

Triggering of earthquakes on upper plate faults during and shortly after recent great (M>8.0) subduction thrust earthquakes raises concerns about earthquake triggering following Cascadia subduction zone earthquakes. Of particular regard to Cascadia was the previously noted, but only qualitatively identified, clustering of M>~6.5 crustal earthquakes in the Puget Sound region between about 1200–900 
Authors
Brian L. Sherrod, Joan Gomberg

Water, ice and mud: Lahars and lahar hazards at ice- and snow-clad volcanoes

Large-volume lahars are significant hazards at ice and snow covered volcanoes. Hot eruptive products produced during explosive eruptions can generate a substantial volume of melt water that quickly evolves into highly mobile flows of ice, sediment and water. At present it is difficult to predict the size of lahars that can form at ice and snow covered volcanoes due to their complex flow character
Authors
Christopher F. Waythomas

Hydrologic monitoring of a landslide-prone hillslope in the Elliott State Forest, Southern Coast Range, Oregon, 2009-2012

The Oregon Coast Range is dissected by numerous unchanneled headwater basins, which can generate shallow landslides and debris flows during heavy or prolonged rainfall. An automated monitoring system was installed in an unchanneled headwater basin to measure rainfall, volumetric water content, groundwater temperature, and pore pressures at 15-minute intervals. The purpose of this report is to
Authors
Joel B. Smith, Jonathan W. Godt, Rex L. Baum, Jeffrey A. Coe, William J. Burns, Michael M. Morse, Basak Sener-Kaya, Murat Kaya

Thermal behavior and ice-table depth within the north polar erg of Mars

We fully resolve a long-standing thermal discrepancy concerning the north polar erg of Mars. Several recent studies have shown that the erg’s thermal properties are consistent with normal basaltic sand overlying shallow ground ice or ice-cemented sand. Our findings bolster that conclusion by thoroughly characterizing the thermal behavior of the erg, demonstrating that other likely forms of physica
Authors
Nathaniel E. Putzig, Michael T. Mellon, Kenneth E. Herkenhoff, Roger J. Phillips, Brian J. Davis, Kenneth J. Ewer, Lauren M. Bowers

Landslides in the northern Colorado Front Range caused by rainfall, September 11-13, 2013

During the second week of September 2013, nearly continuous rainfall caused widespread landslides and flooding in the northern Colorado Front Range. The combination of landslides and flooding was responsible for eight fatalities and caused extensive damage to buildings, highways, and infrastructure. Three fatalities were attributed to a fast moving type of landslide called debris flow. One fatalit
Authors
Jonathan W. Godt, Jeffrey A. Coe, Jason W. Kean, Rex L. Baum, Eric S. Jones, Edwin L. Harp, Dennis M. Staley, William D. Barnhart

Emergency assessment of post-fire debris-flow hazards for the 2013 Springs Fire, Ventura County, California

Wildfire can significantly alter the hydrologic response of a watershed to the extent that even modest rainstorms can produce dangerous flash floods and debris flows. In this report, empirical models are used to predict the probability and magnitude of debris-flow occurrence in response to a 10-year rainstorm for the 2013 Springs fire in Ventura County, California. Overall, the models predict a re
Authors
Dennis M. Staley

Constraining explosive volcanism: Subjective choices during estimates of eruption magnitude

When estimating the magnitude of explosive eruptions from their deposits, individuals make three sets of critical choices with respect to input data: the spacing of sampling sites, the selection of contour intervals to constrain the field measurements, and the hand contouring of thickness/isomass data, respectively. Volcanologists make subjective calls, as there are no accepted published protocols
Authors
Malin Klawonn, Bruce F. Houghton, Don Swanson, Sarah A. Fagents, Paul Wessel, Cecily J. Wolfe

Igneous mineralogy at Bradbury Rise: the first ChemCam campaign at Gale crater

Textural and compositional analyses using ChemCam Remote Micro Imager (RMI) and Laser Induced Breakdown Spectroscopy (LIBS) have been performed on 5 float rocks and coarse gravels along the first 100 meters of the Curiosity traverse at Bradbury rise. ChemCam, the first LIBS instrument sent to another planet, offers the opportunity to assess mineralogic diversity at grain-size scales (∼100μm) and,
Authors
V. Sautter, C. Fabre, O. Forni, M.J. Toplis, A. Cousin, A.M. Ollila, P.-Y. Meslin, S. Maurice, R. C. Wiens, D. Baratoux, N. Mangold, S. Le Mouélic, O. Gasnault, G. Berger, J. Lasue, R.A. Anderson, E. Lewin, M. Schmidt, D. Dyar, B.L. Ehlmann, J. Bridges, B. Clark, P. Pinet

Global surface displacement data for assessing variability of displacement at a point on a fault

This report presents a global dataset of site-specific surface-displacement data on faults. We have compiled estimates of successive displacements attributed to individual earthquakes, mainly paleoearthquakes, at sites where two or more events have been documented, as a basis for analyzing inter-event variability in surface displacement on continental faults. An earlier version of this composite
Authors
Suzanne Hecker, Robert Sickler, Leah Feigelson, Norman Abrahamson, Will Hassett, Carla Rosa, Ann Sanquini

Three-dimensional ground-motion simulations of earthquakes for the Hanford area, Washington

This report describes the results of ground-motion simulations of earthquakes using three-dimensional (3D) and one-dimensional (1D) crustal models conducted for the probabilistic seismic hazard assessment (PSHA) of the Hanford facility, Washington, under the Senior Seismic Hazard Analysis Committee (SSHAC) guidelines. The first portion of this report demonstrates that the 3D seismic velocity model
Authors
Arthur Frankel, Paul Thorne, Alan Rohay

Response of Global Navigation Satellite System receivers to known shaking between 0.2 and 20 Hertz

Over the past decade, several technological advances have allowed Global Navigation Satellite Systems (GNSS) receivers to have the capability to record displacements at high frequencies, with sampling rates approaching 100 samples per second (sps). In addition, communication and computer hardware and software have allowed various institutions, including the U.S. Geological Survey (USGS), to retrie
Authors
John Langbein, John R. Evans, Fredrick Blume, Ingrid Johanson

Geochemical investigation of the hydrothermal system on Akutan Island, Alaska, July 2012

We have studied the geochemistry of the hot springs on Akutan Island in detail for the first time since the early 1980s. Springs in four discrete groups (A-D) along Hot Springs Creek showed generally higher temperatures and substantially higher Na, Ca, and Cl concentrations than previously reported, and total hot-spring discharge has also increased markedly. The springs now account for a heat outp
Authors
D. Bergfeld, Jennifer L. Lewicki, William C. Evans, Andrew G. Hunt, Kinga Revesz, Mark Huebner