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A fault with horizontal movement is called a strike-slip fault. This type of fault occurs when the rocks on either side of the fault move horizontally past each other. Examples of strike-slip faults include the San Andreas Fault in California.
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.
The Hayward Fault is a Strike-slip Fault.
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.
A strike-slip fault has side-to-side movement where the blocks move horizontally past each other. This type of fault is classified as either right-lateral or left-lateral, depending on the direction of movement relative to an observer standing on one of the blocks.
A fault with little or no vertical movement is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past each other, usually in a side-to-side motion. This movement can cause earthquakes when the stress along the fault overcomes friction and the rocks suddenly slip.
A strike-slip fault
A strike slip fault.
a strike slip fault
It is a strike-slip fault.
a strike slip fault
A strike-slip fault