I am sure that the anwser is the San Andreas fault.
The San Andreas fault is a strike-slip fault, where two tectonic plates move horizontally past each other. It is not a reverse fault, where the hanging wall moves up relative to the footwall due to compression.
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.
a normal fault
The maximum ground movement during the 1906 San Francisco earthquake was around 20 feet horizontally along the San Andreas Fault.
A lateral fault is when Shearing causes rock blocks to slide horizontally past each other.
your dad
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.
Dextral fault movements involve horizontal displacement where the right side of the fault moves horizontally relative to the left side. Sinistral fault movements involve horizontal displacement where the left side of the fault moves horizontally relative to the right side. These movements are determined based on the direction of horizontal displacement across the fault plane.
The San Andreas fault is a strike-slip fault, where two tectonic plates move horizontally past each other. It is not a reverse fault, where the hanging wall moves up relative to the footwall due to compression.
The sides of a strike-slip fault move horizontally past each other in a side-to-side motion. This movement can be either left-lateral, where the block opposite an observer moves to the left, or right-lateral, where the block moves to the right.
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.
An oblique slip fault is a type of fault where the movement is a combination of both strike-slip and dip-slip motion. This means that the fault moves both horizontally and vertically. Oblique slip faults are common in areas where different stresses are acting on the Earth's crust, causing complex fault movements.
This is a plate boundary where two tectonic plates moves or slides horizontally past one another with little or no destruction or creation done to the crust.
A fault with horizontal movement is called a strike-slip fault. In strike-slip faults, the movement is primarily horizontal, with one block of rock sliding past the other horizontally. This type of fault is characterized by lateral displacement along the fault line.
Water moves in three directions: downward due to gravity, horizontally as surface runoff, and vertically through infiltration into the ground.
This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.
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.