Generically a "fault" but there could also be an "earthquake" associated with this fracturing.
A fault with where all the movement is horizontal is called a "transverse" fault. but it must be understood that there is a component of horizontal movement associated with Thrust, Reverse and Normal faults too.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
The rock gets farther a part from the fault
Yes, the Whittier fault is a left-lateral strike-slip fault, meaning that the blocks on either side of the fault move horizontally past each other in a left-lateral direction.
The most common type of fault is a strike-slip fault, where two blocks of rock move horizontally past each other. This type of fault is often associated with transform plate boundaries, such as the San Andreas Fault in California.
Strike-slip faults form when rocks along a fault move horizontally past each other, without much vertical movement. These faults are common in transform plate boundaries, where tectonic plates slide past each other horizontally.
The answer is Strike-Slip Fault.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
Reverse
A Strike Slip fault is where the two sides of the fault move past each other horizontally.
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
strike slip fault
The answer is 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.
The rocks move past each other horizontally.
that is the transform boundaries
The rock gets farther a part from the fault
strike slip fault---------------------------------------------------------------------------------------------------------------- BITCHOSAURUS REX