Publications
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Reply to “Comment on ‘Near-surface location, geometry, and velocities of the Santa Monica fault zone, Los Angeles, California’ by R. D. Catchings, G. Gandhok, M. R. Goldman, D. Okaya, M. J. Rymer, and G. W. Bawden” by T. L. Pratt and J. F. Dolan Reply to “Comment on ‘Near-surface location, geometry, and velocities of the Santa Monica fault zone, Los Angeles, California’ by R. D. Catchings, G. Gandhok, M. R. Goldman, D. Okaya, M. J. Rymer, and G. W. Bawden” by T. L. Pratt and J. F. Dolan
In a comment on our 2008 paper (Catchings, Gandhok, et al., 2008) on the Santa Monica fault in Los Angeles, California, Pratt and Dolan (2010) (herein referred to as P&D) cite numerous objections to our work, inferring that our study is flawed. However, as shown in our reply, their objections contradict their own published works, published works of others, and proven seismic...
Authors
Rufus D. Catchings, Michael J. Rymer, Mark R. Goldman, Gerald W. Bawden
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
230Th/U dating of a late Pleistocene alluvial fan along the southern San Andreas fault 230Th/U dating of a late Pleistocene alluvial fan along the southern San Andreas fault
U-series dating of pedogenic carbonate-clast coatings provides a reliable, precise minimum age of 45.1 ± 0.6 ka (2σ) for the T2 geomorphic surface of the Biskra Palms alluvial fan, Coachella Valley, California. Concordant ages for multiple subsamples from individual carbonate coatings provide evidence that the 238U-234U-230Th system has remained closed since carbonate formation. The U...
Authors
Kathryn E.K. Fletcher, Warren D. Sharp, Katherine J. Kendrick, Whitney M. Behr, Kenneth W. Hudnut, Thomas C. Hanks
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
Method for calculating self-noise spectra and operating ranges for seismographic inertial sensors and recorders Method for calculating self-noise spectra and operating ranges for seismographic inertial sensors and recorders
Understanding the performance of sensors and recorders is prerequisite to making appropriate use of them in seismology and earthquake engineering. This paper explores a critical aspect of instrument performance, the “self” noise level of the device and the amplitude range it can usefully record. Self noise limits the smallest signals, while instrument clipping level creates the upper...
Authors
John R. Evans, F. Followill, Charles R. Hutt, R.P. Kromer, R.L. Nigbor, A. T. Ringler, J.M. Steim, E. Wielandt
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
Quasi-periodic recurrence of large earthquakes on the southern San Andreas fault Quasi-periodic recurrence of large earthquakes on the southern San Andreas fault
It has been 153 yr since the last large earthquake on the southern San Andreas fault (California, United States), but the average interseismic interval is only ~100 yr. If the recurrence of large earthquakes is periodic, rather than random or clustered, the length of this period is notable and would generally increase the risk estimated in probabilistic seismic hazard analyses...
Authors
Katherine M. Scharer, Glenn P. Biasi, Ray J. Weldon, Tom E. Fumal
The North American upper mantle: Density, composition, and evolution The North American upper mantle: Density, composition, and evolution
The upper mantle of North America has been well studied using various seismic methods. Here we investigate the density structure of the North American (NA) upper mantle based on the integrative use of the gravity field and seismic data. The basis of our study is the removal of the gravitational effect of the crust to determine the mantle gravity anomalies. The effect of the crust is...
Authors
Walter D. Mooney, Mikhail K. Kaban
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
Observing the Greatest Earthquakes: AGU Chapman Conference on Giant Earthquakes and Their Tsunamis: Viña del Mar and Valparaíso, Chile, 16–20 May 2010 Observing the Greatest Earthquakes: AGU Chapman Conference on Giant Earthquakes and Their Tsunamis: Viña del Mar and Valparaíso, Chile, 16–20 May 2010
An AGU Chapman Conference commemorated the fiftieth anniversary of the 1960 M 9.5 Chile earthquake. Participants reexamined this earthquake, the largest ever recorded instrumentally, and compared it with Chile's February 2010 M 8.8 earthquake. They also addressed the giant earthquake potential of subduction zones worldwide and strategies for reducing losses due to tsunamis. The...
Authors
Brian F. Atwater, Sergio Barrientos, Ines Cifuentes, Marco Cisternas, Kelin Wang