It's a transform boundary between two plates. The resultant fault of a transform boundary.
Strike-Slip fault is the most common fault type in the San Andreas fault system.
Strike-slip faults are the most common fault type around the San Andreas Fault.
It's a transform boundary between two plates. The resultant fault of a transform boundary.
It's a transform boundary between two plates. The resultant fault of a transform boundary.
The transform boundary, where two plates slide past each other.
That would be the San Andreas fault line.
The San Andreas Fault system is primarily a right-lateral strike-slip fault, where the two sides of the fault move horizontally past each other. This fault type is the most prevalent in the system and is responsible for the majority of the movement along the fault.
The most common type of fault in the northern San Andreas Fault system is strike-slip fault, where the blocks move horizontally past each other. This fault system is characterized by lateral movement along the fault line, with the Pacific Plate 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.
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 most studied transform fault in the world is the San Andreas Fault.
There are many faults in California. The two most significant faults are the San Andreas Fault and the Hayward Fault.