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Relationship between the Santa Sonica, Hollywood, and Raymond faults. BY DIEGO FURTADO.

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Presentation on theme: "Relationship between the Santa Sonica, Hollywood, and Raymond faults. BY DIEGO FURTADO."— Presentation transcript:

1 Relationship between the Santa Sonica, Hollywood, and Raymond faults. BY DIEGO FURTADO

2  The “BIG BEND”: Cause of Compression between the Pacific Plate and North American Plate  Mountains and faults are formed: San Gabriel Mountains and Santa Monica Mountains  Transverse Range Southern Boundary Fault System: Extends from east to west unlike other California mountains

3  Base of San Gabriel and Santa Monica Mountains  West- trending system of faults that extends for 200 km  Oblique-slip, reverse-slip, and strike-slip

4 ▼ ▼ ▼ ~900 A.D ~800 A.D. ~1000 A.D 6.0 - 7.0 5.8 – 6.5 6.0 – 7.0 Santa Monica fault connects with Hollywood fault at west Beverly Hills Lineament Hollywood fault likely connects to Raymond fault at Los Angeles River floodplain 0.27 – 0.39 0.33 – 0.75 0.10 - 0.22 40 km 15 km 26 km

5 http://geomaps.wr.usgs.gov/archive/scamp/html/scg_flt.html http://qcode.us/codes/malibu-general-plan/view.php?topic=ii-5_0-5_2-5_2_2&frames=on http://www.data.scec.org Kristin D. Weaver, Paleoseismology and Geomorphology of the Raymond Fault, Los Angeles County, California, Bulletin of the Seismological Society of America pp. 1409–1429, December 2000, P. 1410-1413. James F. Dolan, Eldon M. Gath, Lisa B. Grant, Mark Legg, Scott Lindvall, Karl Mueller, Michael Oskin, Daniel F. Ponti, Charles M. Rubin, Thomas K. Rockwell, John H, Shaw, Jerome A.Treiman, Chris Walls, and Robert S. Yeats (compiler), P. 1-7. James F. Dolan, David D. Bowman, and Charles G. Sammis, Data Repository for “Long range and long term fault intersections in southern California”, Supporting data, references, and notes for paleo-earthquakes in the Los Angeles region.


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