Transform faults are different from convergent and divergent plate boundaries because there is neither the formation nor the destruction of lithosphere at a transform fault, and plate movement is collateral to the length of a transform fault.
A transform fault or transform boundary, occasionally called a strike-slip boundary, is a criticize along a plate boundary where the motion is mainly horizontal.
Transform boundaries is referred to where crust is neither produced nor destroyed as the plates slide horizontally past with one another.
Divergent plate boundaries is referred to where new crust is initiated as the plates pull aside from each other.
Convergent plate boundaries is referred to where crust is demolished as one plate dives below another.
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