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Seismic P-waves are longitudinal waves that can travel through both solids and liquids, while S-waves are transverse waves that can only travel through solids. When an earthquake occurs, P-waves are detected on the opposite side of the Earth, but S-waves are not.

What does this evidence primarily reveal about the Earth's internal structure?

  1. S-waves are actually faster than P-waves, but they are reflected back toward the surface by the extreme gravity at the center of the Earth.
  2. The Earth contains a liquid layer, such as the outer core, that acts as a barrier to S-waves while allowing P-waves to pass through to the other side.
  3. The Earth is composed entirely of solid granite, but S-waves lose all of their energy within the first ten kilometers of the Earth's crust.
  4. Earthquakes only produce S-waves when the tectonic plates are moving horizontally, which explains why they are missing from some detections.

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