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its just like a cracked hard boiled egg the shell are the plates and the egg while is the mantle. the tectonic plates move on top of magma which is the mantle. they move due to convection currents which occur within the mantle the oceanic plates sub duct in to the mantle while the continental plates don't as they are not as dense. they basicly freeze and move sideways and then descend back in to the mantle again just very slowly. just like a massive jigsaw puzzle. if you get a hard boiled egg and crack it and wiggle it around it might become clear!!!

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