Normal faults.
A normal
It is plateaus, seismic waves and/or reverse fault
transform boundary
A fault with hanging walls that move up is called a reverse fault. This type of fault occurs when compressional forces push the rock layers together, causing the hanging wall to be thrust upward relative to the footwall. Reverse faults are commonly associated with convergent plate boundaries, where tectonic plates collide.
This kind of fault is called a normal fault and is usually a sign of crustal extension.
Yes, shearing forces push rocks in different directions along a plane, causing them to slide past each other horizontally. This type of stress typically occurs at transform plate boundaries where tectonic plates slide horizontally past each other.
A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.
Compressional stresses occur at convergent plate boundaries.
The San Andreas Fault is a strike-slip fault, where the movement occurs horizontally along the fault line. It is located in California and is formed by the movement between the Pacific Plate and the North American Plate.
strike-slip faults.
it is a normal fault.
the Hayward fault is a "transform" fault. :)