Seismic waves travel outward from the earthquake's focus, with the epicenter above it. These waves vary in types and speeds, bending and bouncing as they move through different materials.
When earthquakes occur, seismic waves spread out from the focus, with the epicenter being the surface point directly above the focus. These waves include body waves (S- and P-waves) and surface waves, each causing different motions in rocks and traveling at different speeds. The waves bend and bounce, a process known as refraction and reflection, based on the materials they encounter.
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