san gabriel fault

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While rupture on the Sierra Madre fault zone (theoretically) could be limited to one segment at a time, it has recently been suggested that a large event on the San Andreas fault to the north (like that of 1857) could cause simultaneous rupture on reverse faults south of the San Gabriel Mountains -- the Sierra Madre fault zone being a prime example of such. These are not the default projection or datum for most GPS receivers but are the standard for older USGS Topo maps.

The San

A basement boundary between gneissoid rocks of San Gabriel Mountains aspect and Peninsular Ranges rocks strikes east across the basin and connects with the San Jose fault. Volume 46, Number 10

Magnetic polarity stratigraphy dates deposition of the overlying Saugus Formation to between 2.6 Ma and 0.78 Ma.

From 13 million years ago until 4 million years ago, everything south of the San Gabriel fault slid, earthquake by earthquake, a total of about 40 km (24 miles) to the northwest.

The right lateral San Gabriel Fault Zone in southern California extends from the northwestern corner of the Ridge Basin southeastward to the eastern end of the San Gabriel Mountains. The mud pots near the Salton Sea are a result of its action, but your best bet to see the Southern San Andreas Fault … at the San Gabriel fault (an old branch of the San Andreas fault), and terminates in the south at i to 2 km depth at the southern mountain front. The northern and older branch curves eastward in the range interior.

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The San Gabriel fault is ~3 km west of both dams, and is an ~80-km long structure. Reflections on the San Andreas & San Gabriel Faults : striking contradictions to large lateral offsets. The San Andreas Fault begins near the Salton Sea, runs north along the San Bernardino Mountains, crosses Cajon Pass, and then runs along the San Gabriel Mountains east of Los Angeles. A basement boundary between gneissoid rocks of San Gabriel Mountains aspect and Peninsular Ranges rocks strikes east across the basin and connects with the San Jose fault. Close mobile search navigation.

The fault actually crosses the Transverse Ranges, offsetting the San Gabriels from the San Bernardino Mountains at Cajon Pass.

The San Gabriel Basin is a Pliocene-Pleistocene Transverse Ranges structure bounded by the San Gabriel Mountains on the north, the San Jose and Puente Hills on the east, and the Repetto and Montebello Hills on the west. Pyramid and Castaic Dams are in an active transpressional deformation zone between the San Gabriel and San Andreas faults.

The San Andreas fault slices through 600 miles of California, but the most rugged stretch of its path is along the northern edge of the San Gabriel Mountains.
Marine macrofossils from the Gold Canyon beds give an age of 5.2±0.3 Ma by 87 Sr/ 86 Sr analyses. [Robert H Paschall; Henry Walrond] The San Gabriel Fault along the Ridge Basin (GC1W5HG) was created by TerryDad2 on 7/20/2009.

The velocity structure above and below this interface strongly suggests it is the Vincent thrust fault: intermediate velocities (6.2 … The fault is comprised of a series east-west trending faults with a right-lateral strike-slip and with a dip steep to the north. We take the Old Ridge Route over the Liebre Mountains to Quail Lake. San Gabriel Fault Zone, San Gabriel Mountains, California West end from Santa Clara Divide to Red Box Gap DATES 22 May 2000 - 29 May 2000 Note: All coordinate locations are given in UTM Zone 11 North, NAD 1927. It's a Other size geocache, with difficulty of 3.5, terrain of 3. The right lateral San Gabriel Fault Zone in southern California extends from the northwestern corner of the Ridge Basin southeastward to the eastern end of the San Gabriel Mountains. It bifurcates to the southeast in the northwestern San Gabriel Mountains. San Gabriel Fault Zone, San Gabriel Mountains, California West end from Santa Clara Divide to Red Box Gap DATES 22 May 2000 - 29 May 2000 Note: All coordinate locations are given in UTM Zone 11 North, NAD 1927.

The San Gabriel Fault Zone cuts both units. We proceed on Foothill Blvd to Newhall and Castaic Junction. These are not the default projection or datum for most GPS receivers but are the standard for older USGS Topo maps.


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