Faults are cracks or fractures in the Earth's crust caused by stresses that induce brittle deformation of rocks. There are three main types of faults: dip-slip faults which involve vertical motion, strike-slip faults with horizontal motion, and oblique-slip faults with an oblique motion. Normal faults occur during extension while reverse faults are caused by compression. The elastic rebound theory explains that tectonic plates accumulate energy during periods of stress until a sudden slip occurs along the fault, releasing energy in the form of seismic waves and causing earthquakes.