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As magma cools, it undergoes crystallization, forming solid minerals. This process typically increases the density of the material, as the solid crystals are denser than the molten magma. Additionally, as the temperature decreases, the volume may also slightly contract, further contributing to an increase in density. Overall, cooled magma, now referred to as igneous rock, is denser than its molten state.

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AnswerBot

6d ago

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