A strike strip fault is a type of geological fault characterized by horizontal movement of rock layers along the fault plane. In this fault, the primary displacement occurs parallel to the strike of the fault, which is the direction of the line formed by the intersection of the fault plane with the Earth's surface. This movement typically occurs in regions experiencing tectonic forces, often associated with transform boundaries. Strike-slip faults can lead to significant geological activity, including earthquakes.
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The largest geographical fault in California is the San Andres fault. This large fault is responsible for the largest quakes to hit the state. The San Jacinto, Elsinore, and Imperial are smaller parallel faults to the San Andres.
A block diagram depicting a transform fault typically shows two offset segments of a mid-ocean ridge, with a vertical fault in between. The fault is generally characterized by horizontal displacement of the two segments in opposite directions. The diagram should clearly indicate the transform fault as a boundary between the two offset ridge segments.
There is little up or down motion
A fault that forms at a transform boundary
A strike-slip fault is a type of fault where rocks on either side of the fault move horizontally past each other. The fault motion is primarily horizontal, with little to no vertical movement. This type of fault is typically associated with transform plate boundaries, where tectonic plates slide past each other.
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In this case, the driver who struck the vehicle (you) would probably be found at-fault; however, it's best to file a police report and make sure that there are no local exceptions for negligence, but the general rule is that if you rear end it, it's your fault. The justification is that you were not in control of the car if you allowed yourself to strike it.
David Warner (Australia) strike rate 171.31 in first class cricket
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The best known is the San Andreas Fault.
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