* Transform Boundaries: Where Plates Slide Past Each Other Transform boundaries are where tectonic plates slide horizontally past each other. Unlike convergent boundaries (where plates collide) or divergent boundaries (where plates move apart), there's no creation or destruction of crust at transform boundaries.

* What Happens at Transform Boundaries:

* Friction and Earthquakes: The sliding motion creates significant friction, leading to earthquakes. The San Andreas Fault in California is a famous example of a transform boundary.

* Offsetting Features: Transform boundaries can offset other geological features like mid-ocean ridges and mountain ranges.

In summary: Transform boundaries are characterized by the movement of plates past each other, not the creation or destruction of crust.