transform fault

A transform fault is a type of geological boundary where two tectonic plates slide past each other horizontally. Unlike convergent or divergent boundaries, where plates move toward or away from each other, transform faults cause plates to grind against one another. This movement can cause earthquakes as stress builds up and is released. A well-known example is the San Andreas Fault in California. Transform faults play a crucial role in shaping the Earth’s surface and are important for understanding seismic activity.