Surface waves are waves that are essentially confined to the surface of the Earth, in that their amplitudes decrease with depth in some way. This chapter covers the basic theory of such waves, as well as the theory of normal modes, which are waves confined to a surface layer, and are similar to waves in an organ pipe or the motions of a vibrating string fixed at one end or both ends, for instance. Coverage includes Rayleigh waves, which are a combination of compressional and shear waves and produce ground motions parallel to the vertical plane in which the wave is traveling, and are a dominant type of earthquake wave; and Love waves, which are shear waves that produce ground motions in the horizontal plane, and head waves, which are upgoing waves produced by critically refracted transmitted waves. Waves along an interface between two solids are also discussed. Also discussed are how the different frequencies in the wave pulse travel at different wave speeds, and the corresponding concepts of phase and group velocity.In addition, other types of normal modes are covered, as well as an interesting wave phenomenon known as the Airy phase.