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  • P-Waves vs. S-Waves: Understanding Earth's Core Penetration
    The seismic body wave that can penetrate the Earth's core is the P-wave (primary wave).

    Here's why:

    * P-waves are compressional waves, meaning they travel by compressing and expanding the material they pass through. This allows them to travel through both solids and liquids.

    * S-waves (secondary waves) are shear waves, meaning they travel by shaking the material perpendicular to their direction of travel. S-waves can only travel through solids, as liquids cannot support shear stress.

    Since the Earth's outer core is liquid, S-waves cannot pass through it. P-waves, however, can travel through both the solid inner core and the liquid outer core, albeit at a slower speed in the liquid outer core.

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