Observations of surface waves in the 0.001–0.1 Hz band of frequencies can constrain structure of the crust and upper mantle of the Earth, but only body waves provide information on the elastic velocities of the deeper interior of the Earth, all the way to its center.
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Answer:
Observations of surface waves in the 0.001–0.1 Hz band of frequencies can constrain structure of the crust and upper mantle of the Earth, but only body waves provide information on the elastic velocities of the deeper interior of the Earth, all the way to its center.
Explanation:
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Answer:
Body waves reveal the elastic velocities of the Earth's deeper interior, all the way to its core.