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A mantle is a layer inside a planetary body bounded below by a core and above by a crust. Mantles are made of rock or ices, and are generally the largest and most massive layer of the planetary body.
Earth's mantle is a layer of silicate rock between the crust and the outer core. It has a mass of 4.01 × 10 24 kg (8.84 × 10 24 lb) and makes up 67% of the mass of Earth. [ 1 ] It has a thickness of 2,900 kilometers (1,800 mi) [ 1 ] making up about 46% of Earth's radius and 84% of Earth's volume.
30 Απρ 2024 · 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 Earth’s total volume.
The mantle is composed of denser rocks, on which the rocks of the crust float. On geologic timescales, the mantle behaves as a very viscous fluid and responds to stress by flowing. Together the uppermost mantle and the crust act mechanically as a single…
1 Αυγ 2023 · The Mantle. Beneath the crust lies the mantle, extending to a depth of about 2,900 km. It contains silicate rocks that are rich in iron and magnesium. There are two sections of the mantle: the upper mantle, which is more rigid and behaves elastically on short time scales, and the lower mantle, which is solid but flows on geological timescales.
Definition. The mantle is a thick layer of rock located between the Earth's crust and core, comprising about 84% of the Earth's total volume. It plays a crucial role in tectonic activity and the planet's heat transfer processes, affecting everything from volcanic eruptions to plate movements.
The mantle is a thick layer of semi-solid rock located between the Earth's crust and the outer core, extending to about 2,900 kilometers below the surface. This layer plays a crucial role in Earth's internal dynamics, influencing tectonic activity and convection processes that drive plate movements.