This document discusses how the Earth's continents have moved over millions of years due to the movement of tectonic plates. The Earth originally had one supercontinent called Pangaea, but it broke apart as the plates drifted apart slowly over time. There are two types of crust - oceanic and continental. Oceanic crust is thinner and heavier than continental crust. When plates collide at convergent boundaries, the heavier oceanic crust sinks beneath the lighter continental crust, forming volcanoes and trenches. When plates move apart at divergent boundaries, mid-ocean ridges are formed.