shear
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
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.
Strike slip fault - Look it up!
The main difference between a dip-slip fault and a strike-slip fault is the direction of movement. In a dip-slip fault, the movement is primarily vertical along the dip direction of the fault plane, either up or down. In a strike-slip fault, the movement is primarily horizontal along the strike direction of the fault plane, either to the left or right.
No. It is a strike-slip fault.
The fault type that causes rocks to become twisted and strained when they snag each other is a strike-slip fault. In a strike-slip fault, rocks on either side of the fault move horizontally past each other, leading to twisting and straining along the fault zone. This type of movement is typical in transform plate boundaries such as the San Andreas Fault in California.
YES. A Strike-slip fault is usually a transform boundary.
A fault that is a combination of dip-slip and strike-slip movements
A strike slip fault.
The answer is Strike-Slip Fault.
Strike-slip fault -a boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates.