Publications
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Analysis of nonvolcanic tremor on the San Andreas Fault near Parkfield, CA using U.S. Geological Survey Parkfield Seismic Array Analysis of nonvolcanic tremor on the San Andreas Fault near Parkfield, CA using U.S. Geological Survey Parkfield Seismic Array
Reports by Nadeau and Dolenc (2005) that tremor had been detected near Cholame Valley spawned an effort to use UPSAR (U. S. Geological Survey Parkfield Seismic Array) to study characteristics of tremor. UPSAR was modified to record three channels of velocity at 40–50 sps continuously in January 2005 and ran for about 1 month, during which time we recorded numerous episodes of tremor. One...
Authors
Jon B. Fletcher, Lawrence M. Baker
Scientific drilling into the San Andreas Fault Zone Scientific drilling into the San Andreas Fault Zone
This year, the world has faced energetic and destructive earthquakes almost every month. In January, an M = 7.0 event rocked Haiti, killing an estimated 230,000 people. In February, an M = 8.8 earthquake and tsunami claimed over 500 lives and caused billions of dollars of damage in Chile. Fatal earthquakes also occurred in Turkey in March and in China and Mexico in April.
Authors
Mark Zoback, Stephen Hickman, William Ellsworth
Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan Shear-rate-dependent strength control on the dynamics of rainfall-triggered landslides, Tokushima Prefecture, Japan
A typhoon (Typhoon No. 10) attacked Shikoku Island and the Tyugoku area of Japan in 2004. This typhoon produced a new daily precipitation record of 1317 mm on Shikoku Island and triggered hundreds of landslides in Tokushima Prefecture. One catastrophic landslide was triggered in the Shiraishi area of Kisawa village, and destroyed more than 10 houses while also leaving an unstable block...
Authors
G. Wang, A. Suemine, W.H. Schulz
Orientation-independent, nongeometric-mean measures of seismic intensity from two horizontal components of motion Orientation-independent, nongeometric-mean measures of seismic intensity from two horizontal components of motion
New measures of spectral intensity based on the horizontal components of ground shaking are introduced. These new measures are independent of the in situ orientation of the recordings and encompass the full range of spectral amplitudes over all possible rotation angles. Unlike previously introduced measures that are also orientation independent, no geometric means are used in the...
Authors
David M. Boore
Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress
It has been proposed that the crustal stress field contains small-length-scale heterogeneity of much larger amplitude than the uniform background stress. This model predicts that earthquake focal mechanisms should reflect the loading stress rather than the uniform background stress. So, if the heterogeneous stress hypothesis is correct, focal mechanisms before and after a large...
Authors
Jeanne L. Hardebeck
Top of head scarp and internal scarps for landslide deposits in the Little North Santiam River Basin, Oregon Top of head scarp and internal scarps for landslide deposits in the Little North Santiam River Basin, Oregon
Data points represent head scarps, flank scarps, and minor internal scarps (linear) associated with landslide deposits in the Little North Santiam River Basin, Oregon. This work was completed as part of the Master's thesis "Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009...
Authors
Steven Sobieszczyk
Structural geology of Amazonian-aged layered sedimentary deposits in southwest Candor Chasma, Mars Structural geology of Amazonian-aged layered sedimentary deposits in southwest Candor Chasma, Mars
The structural geology of an outcropping of layered sedimentary deposits in southwest Candor Chasma is mapped using two adjacent high-resolution (1 m/pixel) HiRISE digital elevation models and orthoimagery. Analysis of these structural data yields new insight into the depositional and deformational history of these deposits. Bedding in non-deformed areas generally dips toward the center...
Authors
Chris Okubo
The water table The water table
The water table is a fundamental concept in hydrogeology, yet it is frequently incorrectly defined. For example, both the NGWA (2003) and AGI (Neuendorf et al. 2005) glossaries define the water table as the atmospheric pressure surface that is coincident with the top of the zone of saturation. This definition is also found occasionally in groundwater textbooks as well as in primers...
Authors
Thomas L. Holzer
Comment on "Near-surface location, geometry, and velocities of the Santa Monica fault zone, Los Angeles, California" Comment on "Near-surface location, geometry, and velocities of the Santa Monica fault zone, Los Angeles, California"
No abstract available.
Authors
Thomas L. Pratt, James F. Dolan
The GSN and large earthquakes The GSN and large earthquakes
No abstract available.
Authors
Gavin P. Hayes, Hiroo Kanamori, Thorne Lay, Charles J. Ammon
Anomalously low strength of serpentinite sheared against granite and implications for creep on the Hayward and Calaveras Faults Anomalously low strength of serpentinite sheared against granite and implications for creep on the Hayward and Calaveras Faults
Serpentinized ophiolitic rocks are juxtaposed against quartzofeldspathic rocks at depth across considerable portions of the Hayward and Calaveras Faults. The marked compositional contrast between these rock types may contribute to fault creep that has been observed along these faults. To investigate this possibility, we are conducting hydrothermal shearing experiments to look for changes...
Authors
Diane E. Moore, David A. Lockner, David A. Ponce
Analysis of elevation changes detected from multi-temporal LiDAR surveys in forested landslide terrain in western Oregon Analysis of elevation changes detected from multi-temporal LiDAR surveys in forested landslide terrain in western Oregon
We examined elevation changes detected from two successive sets of Light Detection and Ranging (LiDAR) data in the northern Coast Range of Oregon. The first set of LiDAR data was acquired during leafon conditions and the second set during leaf-off conditions. We were able to successfully identify and map active landslides using a differential digital elevation model (DEM) created from...
Authors
W.J. Burns, J. A. Coe, B.S. Kaya, Liwang Ma