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((Short description|Seismic fault in California))
((more citations|date=November 2023))
((Infobox fault|name=Raymond Fault|location=Los Angeles County and Ventura County|state=California|country=USA|named_for=named for Raymond Hill))[[File:USGS - Raymond fault.gif|thumb|The Raymond Fault in Southern California, United States.]]
The '''Raymond Fault''' is a  [[Fault (geology)|fault]] across central [[Los Angeles County, California|Los Angeles County]] and western [[Ventura County, California|Ventura County]] in [[Southern California]].<ref>((Cite web |title=Southern California Earthquake Data Center at Caltech |url=https://scedc.caltech.edu/earthquake/raymond.html |access-date=2023-11-11 |website=scedc.caltech.edu))</ref>

==San Gabriel Valley area==
The eastern end of the Raymond Fault branches from the [[San Andreas Fault]] in the [[San Gabriel Mountains]] where it forms the east fork of the [[San Gabriel River (California)|San Gabriel River]] and [[Monrovia, California|Monrovia]] Canyon. The fault is very straight and follows a [[WbS]] path. It then goes straight west through [[Arcadia, California|Arcadia]] and the [[Santa Anita Racetrack]] in the [[San Gabriel Valley]], and then forms the [[San Rafael Hills]] in [[San Marino, California|San Marino]] and [[South Pasadena, California|South Pasadena]], and Raymond Hill, after which the fault is named.

==Los Angeles–Ventura areas==
The fault continues west to form the hills of [[Highland Park, Los Angeles, California|Highland Park]], the lower eastern Santa Monica Mountains from [[Dodger Stadium]], [[Silver Lake, Los Angeles|Silver Lake]], and [[Griffith Park]] through the [[Hollywood Hills]] above the [[Sunset Strip]] and [[Studio City, California|Studio City]]. Further west the Raymond Fault creates the higher central and western [[Santa Monica Mountains]] from [[Beverly Hills, California|Beverly Hills]] and along the southern [[San Fernando Valley]] to [[Thousand Oaks, California|Thousand Oaks]] and [[Malibu, California|Malibu]], and on to [[Point Mugu]] at the [[Pacific Ocean]]. The fault then continues underwater to form the northern [[Channel Islands (California)|Channel Islands]], and beyond to where it terminates.

==References==
((reflist))

==External links==
* [http://www.data.scec.org/significant/raymond.html Southern California Earthquake Data Center: Raymond Fault]
* [https://web.archive.org/web/20120220013502/http://gldims.cr.usgs.gov/webapps/cfusion/Sites/qfault/qf_web_disp.cfm?disp_cd=C&qfault_or=50&ims_cf_cd=cf USGS Earthquake Hazards Program database: Raymond Fault]

((California Faults))


[[Category:Seismic faults of California]]
[[Category:Geology of Los Angeles County, California]]
[[Category:Geology of Ventura County, California]]
[[Category:Natural history of the Santa Monica Mountains]]
[[Category:Natural history of the Transverse Ranges]]
[[Category:Natural history of Los Angeles County, California]]
[[Category:Natural history of Ventura County, California]]
[[Category:Channel Islands of California]]
[[Category:Geography of the San Fernando Valley]]
[[Category:Geography of the San Gabriel Valley]]

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