Strike Slip Rate
Strike slip fault
When rocks on opposite sides of a fault move in the same direction at different rates, it results in a strike-slip fault. This type of fault occurs when there is horizontal motion along the fault line. The two main types of strike-slip faults are left-lateral and right-lateral, depending on the direction of movement when facing the fault.
This process of rocks moving in opposite directions on opposite sides of a fault is known as strike-slip faulting. The movement can be either left-lateral (sinistral) or right-lateral (dextral), depending on the relative lateral displacement of the blocks. If the rocks move in the same direction but at different rates, it may indicate differential movement caused by friction variations along the fault plane.
Rocks that move in opposite horizontal directions are called strike-slip faults. In these faults, two blocks of rocks slide past each other horizontally along a fault plane in opposite directions. This movement is caused by shear stress in the Earth's crust.
In geology, shearing occurs when rocks slide past each other horizontally in opposite directions. The kind of fault created by shearing is called a strike-slip fault.
strike slip fault
Strike slip fault
strike slip fault
strike slip fault
strike slip fault
strike slip fault
strike slip fault
strike slip fault
strike slip fault
strike slip fault
The rocks on opposite sides of a fault that move in opposite directions or in the same direction at different rates are called fault blocks. These blocks can move horizontally, vertically, or rotationally along the fault line.
Strike-slip fault -a boundary where rocks on opposite sides of the fault move in opposite or the same directions at different rates.