Slab pull primarily occurs at convergent plate boundaries, where one tectonic plate is forced beneath another in a process known as subduction. As the denser oceanic plate descends into the mantle, it pulls the rest of the plate along with it, creating a powerful driving force that contributes to plate tectonics. This phenomenon not only shapes geological features like deep ocean trenches but also influences volcanic activity and earthquakes in the surrounding regions.
Copyright © 2026 eLLeNow.com All Rights Reserved.