Seismotectonics of the Central California Coast Ranges

Shallow geologic structure, offshore Point Arguello to Santa Maria River; central California
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Published:January 01, 1994
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CiteCitation
David Cummings, T. A. Johnson, 1994. "Shallow geologic structure, offshore Point Arguello to Santa Maria River; central California", Seismotectonics of the Central California Coast Ranges, Ina B. Alterman, Richard B. McMullen, Lloyd S. Cluff, D. Burton Slemmons
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This work includes new interpretations of shallow offshore geologic structure between Point Arguello and the Santa Maria River within California’s 3-mi coastal limit. These interpretations are based on multi-sensor high-resolution seismic reflection data collected during January and February 1986.
Water depths within the survey area range from 16 m (50 ft) nearshore to 70 m (230 ft) 3 mi west of Point Arguello. The sea floor slopes between 0.3 and 0.5° south-westward. The thickness of unconsolidated Quaternary sediment in the survey area ranges from 0 (bedrock outcrop) to almost 50 m (165 ft) off Point Arguello.
The survey area crosses...
- active faults
- California
- Central California
- Coast Ranges
- displacements
- earthquakes
- epicenters
- faults
- focal mechanism
- geophysical methods
- geophysical profiles
- geophysical surveys
- Hosgri Fault
- lateral faults
- reflection
- right-lateral faults
- rupture
- seismic methods
- seismic profiles
- seismotectonics
- structural geology
- surveys
- tectonics
- United States
- Santa Maria River
- Point Arguello
- Lions Head Fault
- Purisima Point
- Lompoc-Solvang Fault
- Santa Ynez River fault system
- Pezzoni-Casmalia-Orcutt Fault
- Canada-Honda Fault