are linked there is no change in length. This is due to the plates moving parallel with each other and no new lithosphere is being created to change that length.

Decreasing length faults: In rare cases, transform faults can shrink in length. These occur when two descending subduction plates are linked by a transform fault. In time as the plates are subducted, the transform fault will decrease in length until the transform fault disappears completely, leaving only two subduction zones facing in opposite directions.

Additionally,

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