The area around the San Andreas fault is still experiencing plate tectonic forces. The area to the West is moving in a North West direction while that of the North Western plate is curving down a South Western movement.
The San Andreas is a slipping fault, where two plates slide by each other. Contact tends to hold the edges in place until the pressure builds up to the point that they part with a sudden jerk. That's an earthquake. There will be smaller shocks, called temblors, as the plates settle into a new position, awaiting the next jerk.
Continental
transform boundary
The San Andreas Fault is a transform plate boundary.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.
The San Andreas Fault is a continental transform fault. It is around eight hundred and ten miles long and forms the boundary between the Pacific and the North American lithospheric plates. In California this crack in the crust of the earth is visible. As a result of this fault, many earthquakes have occurred in the regions that it passes.
transform boundary
transform boundary
The kind of fault you may be contemplating about is a transform fault which occurs like all earth quakes when the Earth's tectonic plates move as sea currents change there appearance. A transform fault is the force of two surfaces rubbing across each other creating huge earth quakes like the ones of 1906 and 1989 in San Andreas.
The San Andreas Fault is a transform plate boundary.
Strike-slip
A strike slip fault
thrust or reverse fault,
Normal faults.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
A normal one.