Convergent movement of two plates often results in one plate pushing under another.

This statement accurately describes subduction, which occurs at convergent plate boundaries. When a dense oceanic plate converges with a less dense continental plate, the oceanic plate is forced beneath the continental plate and into the mantle. This process creates deep ocean trenches, volcanic arcs, and can cause powerful earthquakes. The subducting plate melts as it descends, creating magma that rises to form volcanoes.