A transverse fault
Transform or Strike Slip Fault
A strike-slip fault
because of the Andres fault
A strike slip fault.
Yes, a strike-slip fault is caused by shearing.
because of the Andres fault
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
A strike-slip fault is formed from horizontal shearing between plates. This type of fault occurs when the plates move past each other horizontally in opposite directions. Examples include the San Andreas Fault in California.
It is a transform fault where rocks on either side of the fault move sideways past each other. This motion is caused by shearing forces that result in horizontal displacement along the fault line. Examples of transform faults include the San Andreas Fault in California.
Horizontal shearing can result in strike-slip faults, where two plates slide past each other horizontally. This type of fault is common along transform boundaries, such as the San Andreas Fault in California.
A strike-slip fault
The San Andreas Fault is primarily a transform fault formed by lateral shearing, where two tectonic plates slide past each other horizontally. This movement occurs due to the differential motion of the Pacific and North American plates, which creates significant stress and leads to the formation of faults. Over time, the accumulated stress is released through earthquakes, making the San Andreas Fault one of the most studied and well-known fault systems in the world. This shearing action is a key factor in the geological activity of California.