Rayleigh Waves

Rayleigh waves are a type of surface seismic wave that travel along the Earth's surface during an earthquake. They move in a rolling motion, similar to ocean waves, causing both vertical and horizontal ground movement. These waves are slower than other seismic waves but tend to cause the most destruction because their energy is concentrated near the surface, affecting structures and landscapes. Rayleigh waves can travel long distances and are significant in understanding earthquake impacts and constructing resilient buildings.