An earthquake is caused by movements of the earth's crust that occur when plates shift and release potential energy. Most earthquakes result from movements of the earth's crust along faults, as we looked at in Part two of this series. It is along the fault where the rocks first break and move; this point is called the focus and this is where the earthquake begins. The epicenter is the point on the earth's surface directly above the focus. The strongest shaking in an earthquake will be felt at the epicenter. The seismic waves (energy) moves in all directions from the focus.
The energy from an earthquake travels quickly travels outward in waves from the point of breakage. The energy of an earthquake can break and move rock and soil. This energy is measured and scientists use two types of scales to measure earthquakes. The Richter scale measures the magnitude of an earthquake based on the amount of shaking caused by the quake. It is based on energy released by the earthquake. On this scale, each increase of 1 magnitude number equals an increase of 10 in ground motion caused by seismic waves. So, a earthquake with a magnitude of 6 would cause 10 times more ground motion than an earthquake with a magnitude of 5. The Mercalli scale measures the intensity of an earthquake. It is based on personal observations. The intensity of an earthquake includes ground motion and resulting damage.