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primary wave

seismology
Also known as: P wave, compressional wave

Quick Summary

In seismology, seismic waves are vibrations generated by events like earthquakes. The primary wave, or P wave, is a type of body wave that travels through the Earth's interior. It is a longitudinal wave, meaning particles in the medium vibrate back and forth in the same direction as the wave's travel, similar to sound waves. P waves are the fastest seismic waves and can pass through both solids and liquids. They are the first to reach a seismic recording station, originating from the earthquake's focus and traveling towards the epicenter on the surface. These waves are crucial for understanding Earth's internal structure, as their speed and behavior change as they pass through different layers, such as the solid mantle and the liquid outer core.123

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