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The four sub-types of seismic waves are Primary waves (P-waves), Secondary waves (S-waves), Love waves, and Rayleigh waves. P-waves are compressional waves that travel fastest through the Earth, while S-waves are shear waves that move slower and can only travel through solids. Love waves move horizontally and are responsible for much of the damage during an earthquake, and Rayleigh waves create an elliptical rolling motion, affecting both the surface and subsurface. Together, these waves provide critical information about the Earth's structure and behavior during seismic events.

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