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What causes the convection cells in the mantle?
Heat from the core heats up the magma in the mantle. The molecules in the magma move more quickly, taking up more space, thus become less dense. The less dense magma rises upward to the crust. When it gets near the crust, the magma loses it's heat energy and the molecules move less quickly, take up less space, and become more dense. The cooler magma sinks back down towards the mantle and the cycle restarts.