- Garlock Fault
The Garlock Fault is a left-lateral strike-slip fault line running approximately northeast-southwest in southern
California. It runs for much of its length along the southern base of the Tehachapi Mountains. It marks the northern boundary of the area known as the Mojave Block, as well as the southern ends of the Sierra Nevada and the valleys of the westernmost Basin and Range province. Stretching for 250 kilometers, it is the second-longest fault line in California and is one of the most prominent geological features in the southern part of the state.
The Garlock Fault runs from a junction with the
San Andreas Faultin Antelope Valley, eastward to a junction with the Death Valley Fault Zone.
The Garlock is believed to have developed to accommodate the strain differential between the extensional tectonics of the
Great Basincrust and the right lateral strike-slip faulting of the Mohave Desertcrust. [cite web|url=http://books.google.com/books?id=h8fVs7EgaJEC&pg=PA375&lpg=PA375&dq=Garlock+fault+named+for&source=web&ots=WC1GE9ilwn&sig=GxUIAM-_-R4HIu_4juWVm3N1v9g&hl=en#PPA375,M1 |title=Classic Cordilleran Concepts|accessdate=2008-08-10|publisher=Department of Geology, University of Kansas]
Unlike most of the other faults in California, slip on the Garlock Fault is left-lateral; that is, the land on the other side of the fault moves to the left from the perspective of someone facing the fault. In the case of the Garlock Fault, this means that the terrain north of the fault is moving westward relative to the terrain south of the fault, which is moving relatively eastward.
The Garlock moves at a rate of between 2 and 11 millimeters a
year, with an average slip of around 7 millimeters. While most of the fault is locked, certain segments have been shown to move by aseismic creep.
The Garlock is not considered to be a particularly active fault, seldom producing any shaking detectable by humans, although it has been known to generate sympathetic seismic events when triggered by other
earthquakes and in one instance by the removal of ground water. These events, as well as continuing microearthquakeactivity and the state of the scarps from previous ruptures, do indicate that the Garlock will produce another major quake at some point in the future. [cite web|url=http://bssa.geoscienceworld.org/cgi/content/abstract/73/6A/1721 |title=Seismicity of the Garlock fault, California |coauthors=Luciana Astiz and Clarence R. Allen| work=Bulletin of the Seismological Society of America|date=Dec 1983|accessdate=2008-08-10]
The most recent notable event was a magnitude 5.7 near the town of Mojave on
July 11, 1992. It is thought to have been triggered by the Landers Earthquake, just two weeks earlier.
The last significant ruptures on the Garlock were thought to be in the years 1050 A.D. and 1500 A.D.. Research has pinned the interval between significant ruptures on the Garlock as being anywhere between 200 and 3000 years depending on the segment of the fault.
The Garlock constitutes one of the borders of the
Mojave Desert, and is a significant geologic landmark in California. Mountain ranges mark its western edge, and its trace is clearly visible on aerial images of the state.
Relatively few communities lie directly along the Garlock, as it is situated in the desert, Frazier Park, Tehachapi, Mojave, and Johannesburg being the closest. However, a major rupture along the Garlock would probably be felt in most of the southern part of California.
* [http://www.data.scec.org/fault_index/garlock.html Southern California Earthquake Data Center]
* [http://earthquake.usgs.gov/regional/qfaults/ USGS Database]
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