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Furthermore, the mantle is the mostly solid bulk of Earth's interior. The mantle lies between Earth's dense, super-heated core and its thin outer layer, the crust. The mantle is about 2,900 kilometers (1,802 miles) thick, and makes up a whopping 84 percent of Earths total volume. This aspect of Mantle National Geographic Society Offers Significant plays a vital role in practical applications.
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Earth's upper mantle is divided into two major rheological layers the rigid lithospheric mantle (the uppermost mantle), and the more ductile asthenosphere, separated by the lithosphere-asthenosphere boundary. The lithosphere (that is, the lithospheric mantle and the overlying crust) make up tectonic plates, which move over the asthenosphere. This aspect of Mantle National Geographic Society Offers Significant plays a vital role in practical applications.
Furthermore, the mantle is the mostly solid bulk of Earth's interior. The mantle lies between Earth's dense, super-heated core and its thin outer layer, the crust. The mantle is about 2,900 kilometers (1,802 miles) thick, and makes up a whopping 84 percent of Earths total volume. This aspect of Mantle National Geographic Society Offers Significant plays a vital role in practical applications.
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