Earthвђ™s Mantle Is -

: Located between 410 km and 660 km, where extreme pressure causes minerals to change their crystalline structure, becoming much denser.

: 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

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 : Located between 410 km and 660 km,

: 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 Earth's mantle is the massive layer of silicate