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Overview of the 2010 Haiti earthquake Overview of the 2010 Haiti earthquake

The 12 January 2010 Mw 7.0 earthquake in the Republic of Haiti caused an estimated 300,000 deaths, displaced more than a million people, and damaged nearly half of all structures in the epicentral area. We provide an overview of the historical, seismological, geotechnical, structural, lifeline-related, and socioeconomic factors that contributed to the catastrophe. We also describe some...
Authors
Reginald DesRoches, Mary Comerio, Marc Eberhard, Walter D. Mooney, Glenn R. Rix

A Geo-referenced 3D model of the Juan de Fuca Slab and associated seismicity A Geo-referenced 3D model of the Juan de Fuca Slab and associated seismicity

We present a Geographic Information System (GIS) of a new 3-dimensional (3D) model of the subducted Juan de Fuca Plate beneath western North America and associated seismicity of the Cascadia subduction system. The geo-referenced 3D model was constructed from weighted control points that integrate depth information from hypocenter locations and regional seismic velocity studies. We used...
Authors
J.L. Blair, P.A. McCrory, D. H. Oppenheimer, F. Waldhauser

88 hours: The U.S. Geological Survey National Earthquake Information Center response to the March 11, 2011 Mw 9.0 Tohoku earthquake 88 hours: The U.S. Geological Survey National Earthquake Information Center response to the March 11, 2011 Mw 9.0 Tohoku earthquake

The M 9.0 11 March 2011 Tohoku, Japan, earthquake and associated tsunami near the east coast of the island of Honshu caused tens of thousands of deaths and potentially over one trillion dollars in damage, resulting in one of the worst natural disasters ever recorded. The U.S. Geological Survey National Earthquake Information Center (USGS NEIC), through its responsibility to respond to...
Authors
Gavin P. Hayes, Paul S. Earle, Harley M. Benz, David J. Wald, Richard W. Briggs

Ground-Motion Prediction Equations (GMPEs) from a global dataset: The PEER NGA equations Ground-Motion Prediction Equations (GMPEs) from a global dataset: The PEER NGA equations

The PEER NGA ground-motion prediction equations (GMPEs) were derived by five developer teams over several years, resulting in five sets of GMPEs. The teams used various subsets of a global database of ground motions and metadata from shallow earthquakes in tectonically active regions in the development of the equations. Since their publication, the predicted motions from these GMPEs have...
Authors
David M. Boore

The ShakeOut earthquake source and ground motion simulations The ShakeOut earthquake source and ground motion simulations

The ShakeOut Scenario is premised upon the detailed description of a hypothetical Mw 7.8 earthquake on the southern San Andreas Fault and the associated simulated ground motions. The main features of the scenario, such as its endpoints, magnitude, and gross slip distribution, were defined through expert opinion and incorporated information from many previous studies. Slip at smaller...
Authors
R.W. Graves, Douglas B. Houston, K.W. Hudnut

Recently active traces of the Bartlett Springs Fault, California: A digital database Recently active traces of the Bartlett Springs Fault, California: A digital database

The purpose of this map is to show the location of and evidence for recent movement on active fault traces within the Bartlett Springs Fault Zone, California. The location and recency of the mapped traces is primarily based on geomorphic expression of the fault as interpreted from large-scale aerial photography. In a few places, evidence of fault creep and offset Holocene strata in...
Authors
James J. Lienkaemper

Bicentennial of the 1811–1812 New Madrid earthquake sequence, December 2011–2012 Bicentennial of the 1811–1812 New Madrid earthquake sequence, December 2011–2012

A series of earthquakes hit the New Madrid seismic zone of southeastern Missouri, northeastern Arkansas, and adjacent parts of Tennessee and Kentucky, in December 1811 to February 1812. Three earthquakes had a magnitude of 7.0 or greater. The first earthquake occurred December 16, 1811, at 2:15 a.m.; the second 9 a.m. on January 23, 1812; and the third on February 7, 1812, at 3:45 a.m...
Authors
Water Resources Division U.S. Geological Survey

Calculation of aftershock accumulation from observed postseismic deformation: M6 2004 Parkfield, California, earthquake Calculation of aftershock accumulation from observed postseismic deformation: M6 2004 Parkfield, California, earthquake

[1] The postseismic stress accumulation τ(t) over the interval 0.004 to 880 days following the 2004 Parkfield earthquake (M6) can be inferred from GPS measurements of postseismic deformation. The stress relaxation τ(t) − τ′lt, where τ′l is the interseismic loading rate and t is the time after the earthquake, plotted as a function of the number of M > 1.5 aftershocks Na(t) that have...
Authors
James C. Savage

High‐resolution locations of triggered earthquakes and tomographic imaging of Kilauea Volcano's south flank High‐resolution locations of triggered earthquakes and tomographic imaging of Kilauea Volcano's south flank

The spatiotemporal patterns of seismicity beneath Kilauea's south flank give insight to the structure and geometry of the decollement on which large, tsunamigenic earthquakes have occurred, and its relation to slow slip events (SSEs), which have been observed every 1 to 2 years since 1997. In order to record earthquakes triggered by a SSE that was predicted to occur in March 2007, a...
Authors
Ellen M. Syracuse, Clifford H. Thurber, Cecily J. Wolfe, Paul G. Okubo, James H. Foster, Benjamin A. Brooks

Implications of ground-deformation measurements across earth fissures in subsidence areas in the southwestern USA Implications of ground-deformation measurements across earth fissures in subsidence areas in the southwestern USA

Ground deformation was monitored at earth fissures in areas of land subsidence induced by groundwater extraction in the southwestern United States. The ground deformation is consistent with the mechanism that fissures are caused by horizontal strains generated by bending of overburden in response to localized differential compaction. Subsidence profiles indicated that localized...
Authors
Thomas L. Holzer

Earthquakes in the Central United States, 1699-2010 Earthquakes in the Central United States, 1699-2010

This publication is an update of an earlier report, U.S. Geological Survey (USGS) Geologic Investigation I-2812 by Wheeler and others (2003), titled ?Earthquakes in the Central United States-1699-2002.? Like the original poster, the center of the updated poster is a map showing the pattern of earthquake locations in the most seismically active part of the central United States. Arrayed...
Authors
Richard L. Dart, Christina M. Volpi

Modified Mercalli intensity assignments for the May 16, 1909, Northern Plains earthquake Modified Mercalli intensity assignments for the May 16, 1909, Northern Plains earthquake

We use newspaper accounts from the United States and Canada to assign modified Mercalli intensity (MMI) at 90 towns for the May 16, 1909 Northern Plains earthquake. Our MMI assignments generally are consistent with those plotted on Nuttli's (1976) isoseiemal map. The earthquake was felt over more than 1,500,000 km2 in the states of Minnesota, Montana, North Dakota, South Dakota, and...
Authors
W. H. Bakun, M. C. Stickney, G. Rogers, J. Ristau
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