There are two main types of seismic waves: body waves and surface waves. Body waves include P-waves (primary waves) and S-waves (secondary waves), with P-waves traveling faster and able to pass through solids and liquids, while S-waves are slower and can only travel through solids. Surface waves include Love waves and Rayleigh waves, with Love waves moving the ground from side-to-side and Rayleigh waves rolling along the ground like ocean waves, causing both up-down and side-to-side shaking.