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Late quaternary slip-rate variations along the Warm Springs Valley fault system, northern Walker Lane, California-Nevada border Late quaternary slip-rate variations along the Warm Springs Valley fault system, northern Walker Lane, California-Nevada border

The extent to which faults exhibit temporally varying slip rates has important consequences for models of fault mechanics and probabilistic seismic hazard. Here, we explore the temporal behavior of the dextral‐slip Warm Springs Valley fault system, which is part of a network of closely spaced (10–20 km) faults in the northern Walker Lane (California–Nevada border). We develop a late...
Authors
Ryan Gold, Craig dePolo, Richard W. Briggs, Anthony Crone, John Goss

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

Seismicity of the Earth 1900–2010 Middle East and vicinity Seismicity of the Earth 1900–2010 Middle East and vicinity

No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional...
Authors
Jennifer Jenkins, Bethan Turner, Rebecca Turner, Gavin P. Hayes, Sian Davies, Richard L. Dart, Arthur C. Tarr, Antonio Villaseñor, Harley M. Benz

Environmental impact of the landslides caused by the 12 May 2008, Wenchuan, China earthquake Environmental impact of the landslides caused by the 12 May 2008, Wenchuan, China earthquake

The magnitude 7.9 (Mw) Wenchuan, China, earthquake of May 12, 2008 caused at least 88,000 deaths of which one third are estimated to be due to the more than 56,000 earthquake-induced landslides. The affected area is mountainous, featuring densely-vegetated, steep slopes through which narrowly confined rivers and streams flow. Numerous types of landslides occurred in the area, including...
Authors
Lynn M. Highland, Ping Sun

GEM Building Taxonomy (Version 2.0) GEM Building Taxonomy (Version 2.0)

This report documents the development and applications of the Building Taxonomy for the Global Earthquake Model (GEM). The purpose of the GEM Building Taxonomy is to describe and classify buildings in a uniform manner as a key step towards assessing their seismic risk, Criteria for development of the GEM Building Taxonomy were that the Taxonomy be relevant to seismic performance of...
Authors
S. Brzev, C. Scawthorn, A.W. Charleson, L. Allen, M. Greene, Kishor Jaiswal, V. Silva

Metadata for selecting or submitting generic seismic vulnerability functions via GEM's vulnerability database Metadata for selecting or submitting generic seismic vulnerability functions via GEM's vulnerability database

This memo lays out a procedure for the GEM software to offer an available vulnerability function for any acceptable set of attributes that the user specifies for a particular building category. The memo also provides general guidelines on how to submit the vulnerability or fragility functions to the GEM vulnerability repository, stipulating which attributes modelers must provide so that...
Authors
Kishor Jaiswal

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

The effect of complex fault rupture on the distribution of landslides triggered by the 12 January 2010, Haiti earthquake The effect of complex fault rupture on the distribution of landslides triggered by the 12 January 2010, Haiti earthquake

The MW 7.0, 12 January 2010, Haiti earthquake triggered more than 7,000 landslides in the mountainous terrain south of Port-au-Prince over an area that extends approximately 50 km to the east and west from the epicenter and to the southern coast. Most of the triggered landslides were rock and soil slides from 25°–65° slopes within heavily fractured limestone and deeply weathered basalt...
Authors
Edwin L. Harp, Randall W. Jibson, Richard L. Dart

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

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
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