Transform fault

A transform fault or transform boundary, is a fault along a plate boundary where the motion is predominantly horizontal.^[1] It ends abruptly where it connects to another plate boundary, either another transform, a spreading ridge, or a subduction zone.^[2] A transform fault is a special case of a strike-slip fault that also forms a plate boundary.

Most such faults are found in oceanic crust, where they accommodate the lateral offset between segments of divergent boundaries, forming a zigzag pattern. This is a result of oblique seafloor spreading where the direction of motion is not perpendicular to the trend of the overall divergent boundary. A smaller number of such faults are found on land, although these are generally better-known, such as the San Andreas Fault and North Anatolian Fault.