Part 6: Transform Boundaries
Lateral Plate Motion
Transform boundaries accommodate lateral motion between tectonic plates. Unlike divergent and convergent boundaries, crust is neither created nor destroyedβplates slide horizontally past one another along strike-slip faults. These boundaries produce some of the world's most damaging earthquakes and connect segments of mid-ocean ridges.
~1,000 km
San Andreas Length
46 mm/yr
SA Slip Rate
~10β15 km
Seismogenic Depth