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Mantle convection is the slow motion of the Earth's silicate mantle, caused by convection currents that carry heat from the interior to the surface of the Earth. Mantle convection causes the tectonic plates to move around the Earth's surface, causing earthquakes, tsunamis, and volcanic activity.
The process is called mantle convection. This is when the heat from Earth's core causes the mantle to slowly flow, creating currents that can push and move the tectonic plates on the Earth's surface.
Convection currents happen in the mantle and cause tectonic plates to drift. The earth is made up of the iron and nickel core, then the mantle then the crust. And the earths surface is made up of tectonic plates. These plates move due to convection currents.
The movement of the Earth's tectonic plates is primarily driven by the process of mantle convection, where heat from Earth's interior drives the movement of the mantle material. As the mantle material rises and cools near the surface, it moves horizontally and drags the overlying tectonic plates with it. This continuous cycle of rising and sinking material causes the plates to move across Earth's surface.
Mantle convection causes the tectonic plates of the Earth to move slowly. Mantle convection is when heat moves from the mantle to the surface and causes the mantle, and the tectonic plates to move very slowly.