From 1997 to 2000, seismic reflection data from the California Continental Borderland
were acquired to identify the active fault systems in the southern California offshore area. The
studies focused on the coastal zone, which includes the shelf, slope, and adjacent basinal areas,
that poses the greatest potential seismic hazards for the most populated urban corridor along the
U.S. Pacific margin. A major goal is to understand the fault-slip history of, and current strain along,
the active (defined as Holocene age) faults to determine the hazard potential. In addition, the
history of landslide generation is a related focus of the study to determine the potential for
generation of tsunamis that can devastate the coastal area. The primary objective has been
to help mitigate the earthquake hazards for the southern California region by improving our
understanding of how deformation is distributed (spatially and temporally) across the offshore
as well as the onshore regions.
Studies under the Earthquake Hazard Task (the Tierra component of the
CABRILLO Project) focused on
imaging the nearshore fault systems and developing a detailed stratigraphic framework to understand
the late Quaternary history of sedimentation and deformation patterns in the California
Continental Borderland (Figure 1). In addition, seismic-reflection imaging can
provide the subsurface dimensions of the faults and identify the size and frequency of submarine
landslides, both of which are necessary for evaluating the potential for generating destructive
tsunamis in the southern California offshore. In order to evaluate the strain associated with the
offshore structures, the results from the seismic-reflection profiling conducted under this project
will be used to identify possible sites for deployment of acoustic geodetic instruments to monitor
strain in the offshore region. A major goal of mapping under this project is to provide detailed
geologic and geophysical information in GIS data bases that build on the earlier studies and use
the new data to precisely locate active faults and to map recent submarine landslide deposits.
The following sections present the trackline locations, which can be used to link the reader directly
to images of the seismic-reflection profiles; in addition, tables are provided that will allow downloading
the graphical images (both TIFF and JPEG formats) as well as SEG-Y formatted data.