weaves help to determine the structure of the earth
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Core structure Seismology helps us work out the dimensions of the inner and outer core of the Earth. P-waves of a hypothetical earthquake at the North Pole are refracted at the core–mantle boundary, and shadow zones are created. Although P-waves reappear, S-waves do not.
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Explanation: Core structure Seismology helps us work out the dimensions of the inner and outer core of the Earth. P-waves of a hypothetical earthquake at the North Pole are refracted at the core–mantle boundary, and shadow zones are created.
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