The rock gets farther a part from the fault
The rocks move past each other horizontally.
its magma
strike-slip has a horizontal motion
YES. A Strike-slip fault is usually a transform boundary.
A strike-slip fault has little or no vertical movements.
A Transform fault boundaries are where two plates are sliding horizontally past one another. They sometimes even get stuck. the longer the time before the plates slip, the stronger the earthquake.
It is a strike-slip fault.
Crustal plates are grinding past each other in a strike-slip fault.
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 Hayward Fault is a Strike-slip Fault.
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.
Strike slip fault - Look it up!
strike-slip
its a normal fault
strike-slip
it occurs along a transform boundary
strike-slip has a horizontal motion
No. It is a strike-slip fault.
YES. A Strike-slip fault is usually a transform boundary.