Earthвђ™s Mantle Is -

Earth's mantle is the massive layer of silicate rock located between the planet's thin outer crust and its dense, super-heated core. Accounting for about , it is the engine room of our planet, driving the geological processes that shape the surface we live on. Composition and Structure

: Heat from the core creates convection currents in the mantle. These currents act like a conveyor belt, moving tectonic plates, creating mountains, and causing earthquakes. Earth’s mantle is

: Located between 410 km and 660 km, where extreme pressure causes minerals to change their crystalline structure, becoming much denser. Earth's mantle is the massive layer of silicate

: Stretching from 660 km down to the core-mantle boundary, this region is under such immense pressure that the rock remains solid despite temperatures exceeding 3,000°C. Why It Matters These currents act like a conveyor belt, moving

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