Earthquakes occur most frequently at plate boundaries where plates are separating, colliding, or sliding past one another. They also occur along faults within plates. The type and intensity of quakes depends on the plate boundary type. Divergent boundaries see frequent, mild quakes while convergent boundaries experience more intense quakes as pressure builds over time. Transform boundaries produce less predictable quakes ranging from frequent small ones to rare large ones. Magnitude is used to describe earthquake intensity and is measured using the Richter scale. Tsunamis are generated by undersea earthquakes and send waves of water onto coastlines, traveling great distances in short times.