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There are two main types of seismic waves: *body waves* and *surface waves*. Body waves travel through the Earth's interior, while surface waves travel along the surface. Body waves are further divided into P-waves (primary waves) and S-waves (secondary waves). P-waves are the fastest and can travel through solids, liquids, and gases. S-waves are slower and can only travel through solids. Surface waves, which are the ones that cause the most damage, are divided into Love waves and Rayleigh waves. Love waves move the ground side to side, and Rayleigh waves move the ground in an elliptical motion. Knowing about these waves can help you understand how earthquakes affect buildings and the ground around you.
