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Characteristics of the San Andreas Fault Zone. The surface expression of the San Andreas transform fault zone is a right-lateral strike-slip fault. The fault zone is approximately 1300 km long and is made up of three major segments, each with characteristic types, magnitudes and frequencies of earthquake activity.he relative rate of motion between the North American plate and the Pacific plate is approximately 3.5 to 4.6 cm per year, most of which (2.0 to 3.5 cm per year) is accounted for by horizontal displacement along the San Andreas fault zone.
The main characteristic of a reverse fault it that a piece of rock from the plate is thrust up higher than the original level of the ground. This formation is also referred to as a scarp. In contrast, there are two other types of stress, both forming different types of faults. Divergent plate boundaries, which is when the land plates are moving away from each other, experience tensional stress. This type of stress produces normal faults. The rocks and landforms are stretched when tensional stress occurs. Since rocks cannot stretch indefinitely, they eventually break and form a fault.