The relative motion of a plate with respect to a plate is its motion as seen by an observer standing on . The absolute motion of a plate is its motion with respect to a frame attached to the deep Earth, for instance a set of hotspots assumed fixed, or the frame in which the lithosphere as a whole does not turn.
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Example 13.7 (The San Andreas fault)
In central California, at North and West, the rotation poles give the Pacific plate the velocity and the North American plate , in millimetres a year (east, north), in the frame of the whole lithosphere. The Pacific plate relative to North America moves at , that is a year, in a direction west of north (figure below). The San Andreas fault, which runs north-west, carries most of this sliding.