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There are several types of seismic waves that travel at different velocities. P-waves are compressional waves that push and pull particles in the direction of propagation. S-waves are shear waves that involve shearing and rotation of particles perpendicular to the direction of propagation. Surface waves like Rayleigh and Love waves travel along the surface. P-waves travel faster than S-waves. The velocities of seismic waves depend on factors like the material density and elastic properties, saturation level

Author

Intan Nur Dania

Language

EN