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Why are S-waves especially useful in identifying liquid layers of Earth?

Answer and explanation

Correct answer: Because they do not propagate in liquid

The direct answer is B: S-waves do not propagate through liquids. S-waves are secondary or shear waves. In a shear wave, particles must move sideways relative to the direction of travel, so the material must resist shearing. Solids can do this, but liquids cannot maintain a shear shape; therefore S-waves stop at a liquid boundary. Step by step: an earthquake produces waves; S-waves travel through solid rock; when they reach a liquid layer, they cannot continue; the missing S-wave signal helps scientists infer a liquid layer, especially the outer core. Option B is correct. Option A is wrong because S-waves do not become faster in liquid; they cannot pass through it. Option C is wrong because earthquakes occur beneath land and oceans, and S-waves do not originate only in oceans. Option D is wrong because S-waves are seismic waves, not instruments for measuring air temperature. Memory cue: “S means shear and solid”; no shear strength in liquid means no S-wave transmission.

Related tags

S-WavesLiquid-LayerSeismic-Evidence

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