You are right that the Newport-Inglewood fault that runs parallel to the PV fault is much more dangerous. Continues southward as the Palos Verdes - Coronado Bank fault zone.
Additional publication details. The Palos Verdes Hills are part of an uplifted block, with a northwest trend, bounded on the northeast by the Palos Verdes fault zone. The Palos Verdes fault is predominantly a strike-slip fault but has a small vertical component about 10% to 15%. The exact land route of the Palos Verdes Fault has been erased by years of paved streets, housing developments and land modifications, said Tom Henyey, director of the Southern California Earthquake Center at USC. References . The Palos Verdes fault is an oblique-slip fault, with a ratio of strike-slip to dip-slip of 10:1, a relatively small dip-slip component, but yet enough to a) create the Palos Verdes hills, b) uplift the Monterey Formation from a marine to a terrestrial setting and c) create 13 marine terraces via sequential uplift. The Palos Verdes fault (PVF) is an active structure in southern California comprised of several segments that together form a complex fault system. 1) Local map of the South Bay Los Angeles area (directions to each stop are described in detail below).

The Palos Verdes Fault (PVF) is one of few active faults in Southern California that crosses the shoreline and can be studied using both terrestrial and subaqueous methodologies. The Palos Verdes Fault (PVF) is one of few active faults in Southern California that crosses the shoreline and can be studied using both terrestrial and subaqueous methodologies. Cabrillo Fault. GEOLOGY OF THE PALOS VERDES PENINSULA LOS ANGELES CA A FIELD GUIDE FOR THE NON-GEOLOGIST Dr. Brendan McNulty Department of Earth Science California State University Dominguez Hills Project funded the CSUDH Presidential Creative Initiative Fund June 2012 . Depositional Environment. The fault goes out to sea at RAT beach and heads North past Redondo Beach, Hermosa Beach, Manhattan Beach and El Segundo. The Palos Verdes Peninsula is part of an extensive, mostly submarine terrane where Middle Miocene and younger sediments lie unconformably on a tectonically disrupted basement of Mesozoic Catalina Schist (Platt, 1975; Howell and Vedder, 1981).

Depositional Environment. West of the Palos Verdes fault zone, other northwest-striking faults deform the outer shelf and slope. Depositional Environment. You … The magnitude 3.4 temblor, probably associated with the Palos Verdes Fault, hit the area with a sharp punch about 4 p.m. By Josh Grossberg, Daily Breeze Well, it may have been a tiny one, but it was my first and it was due to our own Palos Verdes Fault.

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