Seismic waves are energy waves caused by sudden rock breaks or explosions within the Earth, recorded by seismographs. There are two main types: body waves (primary and secondary) that travel through the Earth, and surface waves (Love and Rayleigh) that move along the surface, causing most earthquake damage. Primary waves compress and pull rocks, secondary waves move side to side, and surface waves create up-and-down motion, with Rayleigh waves being responsible for the most shaking felt during earthquakes.