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The mantle is divided into four main parts from top to bottom: the uppermost mantle, which includes the lithosphere and asthenosphere; the transition zone; the lower mantle; and the outer core. The uppermost mantle is solid and rigid, while the asthenosphere is semi-fluid and allows for tectonic plate movement. The transition zone, located between the upper and lower mantle, features changes in mineral structures due to increased pressure. The lower mantle is solid and extends to the outer core, characterized by higher temperatures and pressures.

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2mo ago

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