transform boundary
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.
The San Andreas Fault was created by a transform boundary, where two tectonic plates slide horizontally past each other. In the case of the San Andreas Fault, the Pacific Plate is moving northwest relative to the North American Plate.
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 Fault is a strike-slip fault where the motion is mainly horizontal, with the two sides moving past each other horizontally. It is a transform boundary between the Pacific Plate and the North American Plate.
The San Andreas fault is a transform boundary, where two tectonic plates slide past each other horizontally. In this case, the Pacific Plate and the North American Plate are moving in opposite directions, causing frequent tremors and earthquakes.
transform boundary
The San Andreas Fault is a transform fault where tectonic plates slide past each other horizontally. The force at the fault is primarily due to the movement of the North American Plate and the Pacific Plate, causing stress to build up until it is released in the form of earthquakes.
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 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
The San Andreas Fault was created by a transform boundary, where two tectonic plates slide horizontally past each other. In the case of the San Andreas Fault, the Pacific Plate is moving northwest relative to the North American Plate.
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.
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.
A normal one.
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.
This kind of fault is called a normal fault and is usually a sign of crustal extension.