Mantle convection is the slow, churning motion of the Earth's mantle caused by heat from the core, which drives the movement of tectonic plates on the Earth's surface. This process is crucial for understanding how heat is transferred within the Earth and how it influences geological activity, including earthquakes and volcanic eruptions. Mantle convection is a key driver in the dynamic behavior of Earth's internal structure and plays a vital role in the formation and movement of plate boundaries.
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