Publications
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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
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
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
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
Constraints on behaviour of a mining‐induced earthquake inferred from laboratory rock mechanics experiments Constraints on behaviour of a mining‐induced earthquake inferred from laboratory rock mechanics experiments
On December 12, 2004, an earthquake of magnitude 2.2, located in the TauTona Gold Mine at a depth of about 3.65 km in the ancient Pretorius fault zone, was recorded by the in-mine borehole seismic network, yielding an excellent set of ground motion data recorded at hypocentral distances of several km. From these data, the seismic moment tensor, indicating mostly normal faulting with a...
Authors
Arthur F. McGarr, Malcolm J. S. Johnston, M. Boettcher, V. Heesakkers, Z. Reches
Comment on “Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region” by U. ten Brink et al. Comment on “Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region” by U. ten Brink et al.
The analysis of historical earthquakes in the northeastern Caribbean by ten Brink et al. [2011, hereafter TB11] addresses the occurrence of large and destructive historical earthquakes associated with the North American-Caribbean plate boundary. One conclusion presented in TB11 is that the recurrence interval for large earthquakes on the left-lateral, strike-slip Septentrional Fault (SF)...
Authors
Carol S. Prentice, Paul Mann, Luis R. Pena
Triggered tremor sweet spots in Alaska Triggered tremor sweet spots in Alaska
To better understand what controls fault slip along plate boundaries, we have exploited the abundance of seismic and geodetic data available from the richly varied tectonic environments composing Alaska. A search for tremor triggered by 11 large earthquakes throughout all of seismically monitored Alaska reveals two tremor “sweet spots”—regions where large-amplitude seismic waves...
Authors
Joan Gomberg, Stephanie Prejean
Assessing the location and magnitude of the 20 October 1870 Charlevoix, Quebec, earthquake Assessing the location and magnitude of the 20 October 1870 Charlevoix, Quebec, earthquake
The Charlevoix, Quebec, earthquake of 20 October 1870 caused damage to several towns in Quebec and was felt throughout much of southeastern Canada and along the U.S. Atlantic seaboard from Maine to Maryland. Site‐specific damage and felt reports from Canadian and U.S. cities and towns were used in analyses of the location and magnitude of the earthquake. The macroseismic center of the...
Authors
John E. Ebel, Megan Dupuy, William H. Bakun
The effect of sampling rate and anti-aliasing filters on high-frequency response spectra The effect of sampling rate and anti-aliasing filters on high-frequency response spectra
The most commonly used intensity measure in ground-motion prediction equations is the pseudo-absolute response spectral acceleration (PSA), for response periods from 0.01 to 10 s (or frequencies from 0.1 to 100 Hz). PSAs are often derived from recorded ground motions, and these motions are usually filtered to remove high and low frequencies before the PSAs are computed. In this article...
Authors
David M. Boore, Christine Goulet
New Zealand’s deadliest quake sounds alarm for cities on fault lines New Zealand’s deadliest quake sounds alarm for cities on fault lines
The catastrophic Christ Church Earthquake is a strong reminder to engineers and scientists of the hazards pose by fault lines, both mapped and unknown, near major cities. In February 2011, the relatively moderate earthquake that struck the cities of Christchurch and Lyttleton in the Canterbury region of New Zealand's South Island surprised many with its destructive power. The magnitude 6...
Authors
Erol Kalkan