site notes that the roughly 50-mile-long fault line continues southward, offshore, as the Palos Verdes-Coronado Bank Fault Zone.
Then around 2 MYA the vertical slips on the fault raised the knoll above sea level and the Palos Verdes Island emerged. Palos Verdes Fault An offshore fault that mostly travels along the Orange County coast, the Palos Verdes Fault runs aground right through the Port of Los Angeles.
The Palos Verdes Fault (PVF) is an active northwest‐southeast trending right‐lateral strike‐slip fault that involves onshore and offshore sections, extending from northern Santa Monica Bay, across the Palos Verdes Peninsula, and offshore again across the San Pedro Shelf and Slope (Figure 1). 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). The Palos Verdes fault (PVF) is an active structure in southern California comprised of several segments that together form a complex fault system. The fault has been active since the Miocene and is a major regional seismic source. References . The Palos Verdes Fault Zone, which traverses the southern portion of the South Bay, has two branches - the Cabrillo Fault and the Redondo Canyon Fault - which join the main fault at different points along its route. In 2017, the USGS gave a report on a hypothetical M7.3 earthquake on the Palos Verdes Fault that would deliver a “direct hit” on the port, estimating that it would kill 200 people and decimate over 2,000 buildings. You … It is believed that the island has been rising … Type of Faulting: right-normal (?) Fig. 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. 1) Local map of the South Bay Los Angeles area (directions to each stop are described in detail below). 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. According to a Southern California Earthquake Center scientist interviewed for a previous Ask Us column, the P.V. 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. Palos Verdes is much safer than the LA Basin as you said.
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 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. An offshore fault that mostly travels along the Orange County coast, the Palos Verdes Fault runs aground right through the Port of Los Angeles.
Lying along the westernmost border of the Los Angeles Basin, the Palos Verdes Peninsula provides a unique opportunity to examine the complex tectono-stratigraphic history of the Los Angeles Basin/Inner Borderland region.
West of the Palos Verdes fault zone, other northwest-striking faults deform the outer shelf and slope. Continues southward as the Palos Verdes - Coronado Bank fault zone. The largest earthquake within 30 miles of Rancho Palos Verdes, CA was a 5.7 Magnitude in 1987.
Additional publication details. Cabrillo Fault.
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