The document summarizes the theory of plate tectonics. It explains that the Earth's crust is broken into plates that are constantly moving due to convection currents in the mantle. There are three main types of plate boundaries: divergent where plates pull apart and new crust is formed; convergent where plates crash together and can cause volcanic activity and mountain building; and transform where plates slide past each other and can cause earthquakes. The theory integrated the earlier concepts of continental drift, which proposed the slow drifting of continents, and seafloor spreading, which showed new crust was forming under the oceans. Together, these theories explained how plate tectonics shapes the Earth's surface over millions of years through volcanic and seismic activity