Publications
Filter Total Items: 2057
Size distribution of Parkfield’s microearthquakes reflects changes in surface creep rate Size distribution of Parkfield’s microearthquakes reflects changes in surface creep rate
The nucleation area of the series of M6 events in Parkfield has been shown to be characterized by low b-values throughout the seismic cycle. Since low b-values represent high differential stresses, the asperity structure seems to be always stably stressed and even unaffected by the latest main shock in 2004. However, because fault loading rates and applied shear stress vary with time...
Authors
Theresa Tormann, Stefan Wiemer, Sabrina Metzger, Andrew J. Michael, Jeanne L. Hardebeck
Near real-time monitoring of volcanic surface deformation from GPS measurements at Long Valley Caldera, California Near real-time monitoring of volcanic surface deformation from GPS measurements at Long Valley Caldera, California
Long Valley Caldera in eastern California is an active volcanic area and has shown continued unrest in the last three decades. We have monitored surface deformation from Global Positioning System (GPS) data by using a projection method that we call Targeted Projection Operator (TPO). TPO projects residual time series with secular rates and periodic terms removed onto a predefined spatial...
Authors
Kang Hyeun Ji, Thomas A. Herring, Andrea L. Llenos
Implications of the Mw9.0 Tohoku-Oki earthquake for ground motion scaling with source, path, and site parameters Implications of the Mw9.0 Tohoku-Oki earthquake for ground motion scaling with source, path, and site parameters
The Mw9.0 Tohoku-oki Japan earthquake produced approximately 2,000 ground motion recordings. We consider 1,238 three-component accelerograms corrected with component-specific low-cut filters. The recordings have rupture distances between 44 km and 1,000 km, time-averaged shear wave velocities of VS30 = 90 m/s to 1,900 m/s, and usable response spectral periods of 0.01 sec to >10 sec. The...
Authors
Jonathan P. Stewart, Saburoh Midorikawa, Robert W. Graves, Khatareh Khodaverdi, Tadahiro Kishida, Hiroyuki Miura, Yousef Bozorgnia, Kenneth W. Campbell
Global earthquake fatalities and population Global earthquake fatalities and population
Modern global earthquake fatalities can be separated into two components: (1) fatalities from an approximately constant annual background rate that is independent of world population growth and (2) fatalities caused by earthquakes with large human death tolls, the frequency of which is dependent on world population. Earthquakes with death tolls greater than 100,000 (and 50,000) have...
Authors
Thomas L. Holzer, James C. Savage
Working with strainmeter data Working with strainmeter data
The Plate Boundary Observatory (PBO), the geodetic component of the U.S. National Science Foundation–funded Earthscope program, includes 75 borehole and 6 laser strainmeters (http://pbo.unavco.org). The strainmeters are installed at several locations: on the Cascadia forearc in Washington state and on Vancouver Island, Canada; in arrays of two to nine instruments along the North American...
Authors
Kathleen M. Hodgkinson, Duncan Agnew, Evelyn A. Roeloffs
Site Response and Basin Waves in the Sacramento–San Joaquin Delta, California Site Response and Basin Waves in the Sacramento–San Joaquin Delta, California
The Sacramento–San Joaquin Delta is an inland delta at the western extent of the Central Valley. Levees were built around swampy islands starting after the Civil War to reclaim these lands for farming. Various studies show that these levees could fail in concert from shaking from a major local or regional earthquake resulting in salty water from the San Francisco Bay contaminating the...
Authors
Jon Peter B. Fletcher, John Boatwright
Clustering of GPS velocities in the Mojave Block, southeastern California Clustering of GPS velocities in the Mojave Block, southeastern California
We find subdivisions within the Mojave Block using cluster analysis to identify groupings in the velocities observed at GPS stations there. The clusters are represented on a fault map by symbols located at the positions of the GPS stations, each symbol representing the cluster to which the velocity of that GPS station belongs. Fault systems that separate the clusters are readily...
Authors
James C. Savage, Robert W. Simpson
U.S. Geological Survey natural hazards science strategy— Promoting the safety, security, and economic well-being of the Nation U.S. Geological Survey natural hazards science strategy— Promoting the safety, security, and economic well-being of the Nation
Executive Summary The mission of the U.S. Geological Survey (USGS) in natural hazards is to develop and apply hazard science to help protect the safety, security, and economic well-being of the Nation. The costs and consequences of natural hazards can be enormous, and each year more people and infrastructure are at risk. USGS scientific research—founded on detailed observations and...
Authors
Robert R. Holmes, Lucile M. Jones, Jeffery C. Eidenshink, Jonathan W. Godt, Stephen H. Kirby, Jeffrey J. Love, Christina A. Neal, Nathaniel G. Plant, Michael L. Plunkett, Craig S. Weaver, Anne Wein, Suzanne C. Perry
NGA-West 2 Equations for predicting PGA, PGV, and 5%-Damped PSA for shallow crustal earthquakes NGA-West 2 Equations for predicting PGA, PGV, and 5%-Damped PSA for shallow crustal earthquakes
We provide ground-motion prediction equations for computing medians and standard deviations of average horizontal component intensity measures (IMs) for shallow crustal earthquakes in active tectonic regions. The equations were derived from a global database with M 3.0–7.9 events. We derived equations for the primary M- and distance-dependence of the IMs after fixing the VS30-based...
Authors
David M. Boore, Jon P. Stewart, Emel Seyhan, Gail M. Atkinson
Origin of the Blytheville Arch, and long-term displacement on the New Madrid seismic zone, central United States Origin of the Blytheville Arch, and long-term displacement on the New Madrid seismic zone, central United States
The southern arm of the New Madrid seismic zone of the central United States coincides with the buried, ~110 km by ~20 km Blytheville Arch antiform within the Cambrian–Ordovician Reelfoot rift graben. The Blytheville Arch has been interpreted at various times as a compressive structure, an igneous intrusion, or a sediment diapir. Reprocessed industry seismic-reflection profiles presented...
Authors
Thomas L. Pratt, Robert Williams, Jackson K. Odum, William J. Stephenson
Weakening of ice by magnesium perchlorate hydrate Weakening of ice by magnesium perchlorate hydrate
We show that perchlorate hydrates, which have been detected at high circumpolar martian latitudes, have a dramatic effect upon the rheological behavior of polycrystalline water ice under conditions applicable to the North Polar Layered Deposits (NPLD). We conducted subsolidus creep tests on mixtures of ice and magnesium perchlorate hydrate, Mg(ClO4)2·6H2O (MP6), of 0.02, 0.05, 0.10, and...
Authors
Hendrick J. Lenferinka, William B. Durhama, Laura A. Sternb, Asmin V. Patharec
Megacity megaquakes—Two near misses Megacity megaquakes—Two near misses
Two recent earthquakes left their mark on Santiago de Chile and Tokyo, well beyond the rupture zones, raising questions about the future vulnerability of these and other cities that lie in seismically active regions. Though spared strong shaking, the megacities nevertheless lit up in small quakes, perhaps signaling an abrupt change in the condition for failure on the faults beneath the...
Authors
Ross S. Stein, Shinji Toda