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Mantle (geology) wikipedia. The interior of earth, much like the other terrestrial planets, is divided into layers of various composition. The mantle is a layer between the crust and the. Earth’s interior shape page 1 of twenty-two purdue university. Earth’s interior structure page 2 of 22 method draw a mild middle line transition quarter, and density of rocks with depth through the earth). Structure of the earth wikipedia. The interior shape of the earth is layered in spherical shells. Those layers can be described through their chemical and their rheological houses. Mohorovicic discontinuity the moho geology and earth. How deep is the moho? The mohorovicic discontinuity marks the decrease restriction of earth's crust. As said above, it occurs at a mean intensity of approximately eight kilometers. Mohorovicic discontinuity the moho geology and earth. How deep is the moho? The mohorovicic discontinuity marks the lower restriction of earth's crust. As stated above, it takes place at a median intensity of about eight kilometers.
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