Strike-slip faults indicate rocks are sliding past each other horizontally, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.
strike-slip
a strike-slip fault
We can find strike slip fault between two tectonic plates. For exemple; San Andreas fault in California is a strike slip fault and represent the limit between America plate and Pacifique plate. These two plates move with an inverse movement(~1 towards the north and ~1 toward the south). But we can also find this kind of fault in other context like in a colision.
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
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 certain type of strike-slip fault is found at a transform plate boundary.
strike-slip
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.
strike-slip
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
Strike-slip
a strike-slip fault
Strike-Slip Faulting
They can cause earthquakes or plate movements, depends how big it was. -bkinishi@yahoo.com
The San Andreas fault is an example of a strike-slip fault. It is located at a transform boundary, and was created when the Pacific plate and North American plate ground past one another horizontally.