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  Garnet Hill Fault

TYPE OF FAULTING: right-lateral strike-slip - ANIMATION
but evolves into oblique right-reverse at extreme western end
LENGTH: 25 km
NEARBY COMMUNITIES: White Water, North Palm Springs, Palm Springs
MOST RECENT SURFACE RUPTURE: Holocene at western end; otherwise, Late Quaternary
SLIP RATE: estimated at 10 to 20 percent of the slip rate of the Banning fault
INTERVAL BETWEEN MAJOR RUPTURES: unknown
PROBABLE MAGNITUDES: MW 6.0 - 7.0, alone;
might ruputure along with nearby faults
DIP: The Garnet Hill fault dips to the north.
OTHER NOTES: Displayed ground cracking along surface trace after the 1986 North Palm Springs earthquake. This was not surface rupture, however, but was due to strong shaking.

Map of locality

REFERENCES


This fault is featured on the following map:

Southern Fault Map

San Gorgonio Pass Fault Map