The goal is to learn the timing of recent faulting events, whether slip rates can be determined, and whether synchronous sediment transport events took place within multiple canyons indicating triggering by large prehistoric
earthquake events.
Location
southern California, United States, Pacific Ocean
Summary
Collected push cores and vibracores from the La Jolla fan and San Diego Trough
Info derived
Sediment deposition rates and timing of movement on faults
