The Garlock Fault is a left-lateral strike-slip fault running northeast-southwest along the north margins of the Mojave Desert of Southern California, for much of its length along the southern base of the Tehachapi Mountains.
The Garlock Fault is a left-lateral strike-slip fault. This is for much. This left-lateral strike-slip fault is running northeast-southwest along the north margins of the Mojave Desert of Southern California of its length along the southern base of the Tehachapi Mountains.