Publications
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Analysis of tests of subsurface injection, storage, and recovery of freshwater in Lancaster, Antelope Valley, California Analysis of tests of subsurface injection, storage, and recovery of freshwater in Lancaster, Antelope Valley, California
Ground-water levels in Lancaster, California, declined more than 200 feet during the 20th century, resulting in reduced ground-water supplies and more than 6 feet of land subsidence. Facing continuing population growth, water managers are seeking solutions to these problems. Injection of imported, treated fresh water into the aquifer system when it is most available and least expensive...
Authors
Steven P. Phillips, Carl S. Carlson, Loren F. Metzger, James F. Howle, Devin L. Galloway, Michelle Sneed, Marti E. Ikehara, Kenneth W. Hudnut, Nancy E. King
Is a powerful quake likely to strike in the next 30 years? Is a powerful quake likely to strike in the next 30 years?
No abstract available.
Authors
Andrew J. Michael, Stephanie L. Ross, Robert W. Simpson, Mary Lou Zoback, David P. Schwartz, Michael L. Blanpied
Earthquake recordings from the 2002 Seattle Seismic Hazard Investigation of Puget Sound (SHIPS), Washington state Earthquake recordings from the 2002 Seattle Seismic Hazard Investigation of Puget Sound (SHIPS), Washington state
This report describes seismic data obtained during the fourth Seismic Hazard Investigation of Puget Sound (SHIPS) experiment, termed Seattle SHIPS . The experiment was designed to study the influence of the Seattle sedimentary basin on ground shaking during earthquakes. To accomplish this, we deployed seismometers over the basin to record local earthquakes, quarry blasts, and teleseisms...
Authors
Thomas L. Pratt, Karen L. Meagher, Thomas M. Brocher, Thomas Yelin, Robert Norris, Lynn Hultgrien, Elizabeth Barnett, Craig S. Weaver
Lithospheric buoyancy and continental intraplate stresses Lithospheric buoyancy and continental intraplate stresses
Lithospheric buoyancy, the product of lithospheric density and thickness, is an important physical property that influences both the long-term stability of continents and their state of stress. We have determined lithospheric buoyancy by applying the simple isostatic model of Lachenbruch and Morgan (1990). We determine the crustal portion of lithospheric buoyancy using the USGS global...
Authors
M.L. Zoback, Walter D. Mooney
Observing earthquakes triggered in the near field by dynamic deformations Observing earthquakes triggered in the near field by dynamic deformations
We examine the hypothesis that dynamic deformations associated with seismic waves trigger earthquakes in many tectonic environments. Our analysis focuses on seismicity at close range (within the aftershock zone), complementing published studies of long-range triggering. Our results suggest that dynamic triggering is not confined to remote distances or to geothermal and volcanic regions...
Authors
Joan S. Gomberg, P. Bodin, P.A. Reasenberg
Cold cratonic roots and thermal blankets: How continents affect mantle convection Cold cratonic roots and thermal blankets: How continents affect mantle convection
Two-dimensional convection models with moving continents show that continents profoundly affect the pattern of mantle convection. If the continents are wider than the wavelength of the convection cells (-3000 km, the thickness of the mantle), they cause neighboring deep mantle thermal upwellings to coalesce into a single focused upwelling. This focused upwelling zone will have a...
Authors
V.P. Trubitsyn, Walter D. Mooney, D.H. Abbott
Source model for the Mw 6.7, 23 October 2002, Nenana Mountain earthquake (Alaska) from InSAR Source model for the Mw 6.7, 23 October 2002, Nenana Mountain earthquake (Alaska) from InSAR
The 23 October 2002 Nenana Mountain Earthquake (Mw ∼ 6.7) occurred on the Denali Fault (Alaska), to the west of the Mw ∼ 7.9 Denali Earthquake that ruptured the same fault 11 days later. We used 6 interferograms, constructed using radar images from the Canadian Radarsat-1 and European ERS-2 satellites, to determine the coseismic surface deformation and a source model. Data were acquired...
Authors
Tim J. Wright, Z. Lu, Charles Wicks
Natural weathering rates of silicate minerals Natural weathering rates of silicate minerals
No abstract available.
Authors
A. F. White
Comments on potential geologic and seismic hazards affecting Mare Island, Solano County, California Comments on potential geologic and seismic hazards affecting Mare Island, Solano County, California
This report was prepared in response to a written request from the City of Vallejo, California, to the U.S. Geological Survey (USGS). By letter of October 4, 2002, the City requested that the USGS "provide advice to the City’s LNG Health and Safety Committee on its review of a potential liquid natural gas project" on the southern portion of Mare Island. The City specifically requested...
Authors
T.L. Holzer, C. M. Wentworth, W. H. Bakun, J. Boatwright, T.E. Brocher, M. Çelebi, W.L. Ellsworth, J.P.B. Fletcher, E.L. Geist, R. W. Graymer, R. E. Kayen, D. K. Keefer, D. H. Oppenheimer, W.U. Savage, David P. Schwartz, R.W. Simpson
Earthquake-volcano interactions Earthquake-volcano interactions
No abstract available.
Authors
David P. Hill, Frederick Pollitz, Christopher Newhall
Felt reports and intensity assignments for aftershocks and triggered events of the great 1906 California earthquake Felt reports and intensity assignments for aftershocks and triggered events of the great 1906 California earthquake
The San Andreas fault is the longest fault in California and one of the longest strikeslip faults in the world, yet little is known about the aftershocks following the most recent great event on the San Andreas, the M 7.8 San Francisco earthquake, on 18 April 1906. This open-file report is a compilation of first-hand accounts (felt reports) describing aftershocks and triggered events of...
Authors
Aron J. Meltzner, David J. Wald
Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 2000 through December 31, 2001 Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 2000 through December 31, 2001
The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained seismic monitoring networks at potentially active volcanoes in Alaska since 1988 (Power and others, 1993; Jolly and others, 1996; Jolly and others, 2001)...
Authors
James P. Dixon, Scott D. Stihler, John A. Power, Guy Tytgat, Steve Estes, Seth C. Moran, John Paskievitch, Stephen R. McNutt