The Wilmington blind thrust fault may represent one of the largest deterministic seismic hazards in the United States, in that it extends for more than 30 km along strike beneath the densely populated Los Angeles metropolitan area and the Ports of Los Angeles and Long Beach.

Blind thrust faults Edit. Some faults are actually composed of several fractures called ... A thrust fault is a reverse fault with a gently-dipping fault surface. Because of the lack of surface evidence, blind thrust faults are difficult to detect until they rupture.
California Has Its Faults From January/February 1992 issue of California Geology magazine A fault is a fracture along which there is movement.

If the fault plane terminates before it reaches the Earth's surface, it is referred to as a blind thrust fault. It is unclear if the Santa Monica fault and the blind thrust are the same fault, or if the two faults represent strain partitioning. This map is not meant to be used as a zoning guide, nor for risk assessment. If the fault plane terminates before it reaches the Earth's surface, it is referred to as a blind thrust fault. Numerous examples in the Rockies and Appalachians.

While strike-slip faults occur across the world, the most famous is the San Andreas fault. This type of faulting is common in areas of compression, such as regions where one plate is being subducted under another as in Japan. Present-day examples include the. California Has Its Faults From January/February 1992 issue of California Geology magazine A fault is a fracture along which there is movement. Others are underground, with nothing on the surface revealing their presence (a blind thrust fault).

Indeed, since these maps show only surface traces of faults, some potentially damaging faults -- namely, blind thrust faults, like the one which caused the Northridge earthquake of 1994-- are not shown.

We demonstrate that the Compton blind-thrust fault is active and has generated at least six large-magnitude earthquakes (Mw 7.0-7.4) during the past 14,000 years.

If the 0.6 mm/yr dip-slip rate is the same as that on the blind thrust, then north-south shortening on the entire structure is 0.4 mm/yr (Dolan et al., 2000a).
The 1994 Northridge earthquake was caused by a blind thrust fault. Strike-slip systems Occurrence of strike-slip tectonics Major continental transform faults. For one, there’s the type of motion thrust faults produce, which is more of a vertical shove than the horizontal back and forth of a strike-slip fault, Wolfe says. Faults and Active Tectonics Evidence of faulting can be seen throughout the Mojave region. Subduction zones are a special class of thrusts that form the largest faults on Earth and give rise to the largest earthquakes. Hollywood fault

Information available includes the age of the most recent activity on each fault segment, surface rupture areas, and whether or not the faults are visible at the surface. Some faults are well known and easy to spot, such as the San Andreas.

Collectively the branches are a fault zone (see map).




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