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Body waves are seismic waves that travel through the Earth's interior. The two main types are P (primary) waves and S (secondary) waves.12

P waves are longitudinal waves, meaning particles vibrate parallel to the wave's direction of travel. They are the fastest seismic waves and can pass through solids and liquids.12

S waves are transverse waves, where particles vibrate perpendicular to the wave's direction of travel. They are slower than P waves and can only travel through solid material.12

Seismologists use the travel times and characteristics of these body waves, recorded by seismographs, to study the Earth's deep structure and composition.32

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