- San Gabriel Fault
The San Gabriel Fault is a geological fault that forms the boundary of the southern portion of the San Gabriel Mountains and running about 87
mile s (140kilometer s). The fault is a right-lateral strike-slip that was last active 1,000 of years ago (Late Quaternary west of intersection with theSierra Madre fault ; Quaternary east of that intersection; Holocene only between Saugus and Castaic). It extends southeastward fromRidge Basin to the westernSan Gabriel Mountains .outhern and northern segments
It was once part of the
San Andreas Fault , and is believed to be the former path of the San Andreas. It is also believed that the northwestern end of the fault zone meets the current San Andreas Fault beneath theFrazier Mountain Thrust (near the juncture of the San Andreas with the Garlock andBig Pine Fault s). [ [http://quake.usgs.gov/info/faultmaps/fault213.html San Gabriel fault zone ] ]Activity in the San Gabriel Fault
The San Gabriel moves at a rate of between 1 and 5 millimeters a
year , with an average slip of around 3 millimeters.ee also
*
Earthquake
* Richter scale
*Plate tectonics
*Geology
*Seismology
*Seismic retrofit
*Southern California External links
*http://geomaps.wr.usgs.gov/socal/geology/inland_empire/ie_san_gabriel_fault.html
*http://aapgbull.geoscienceworld.org/cgi/content/abstract/46/10/1938
*http://www.data.scec.org/fault_index/gabriel.htmlReferences
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