When an earthquake occurs the seismic waves (P and S waves) spread out in all directions through the Earth's interior. ... Seismic waves move more slowly through a liquid than a solid. Molten areas within the Earth slow down P waves and stop S waves because their shearing motion cannot be transmitted through a liquid.
Earthquakes radiate seismic energy as both body and surface waves. Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. ... The P wave can move through solid rock and fluids, like water or the liquid layers of the earth.
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When an earthquake occurs the seismic waves (P and S waves) spread out in all directions through the Earth's interior. ... Seismic waves move more slowly through a liquid than a solid. Molten areas within the Earth slow down P waves and stop S waves because their shearing motion cannot be transmitted through a liquid.
Answer:
Earthquakes radiate seismic energy as both body and surface waves. Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. ... The P wave can move through solid rock and fluids, like water or the liquid layers of the earth.
Explanation:
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