Crystallization in the rock cycle refers to the process of solidifying magma into igneous rocks through the formation of crystal structures. When magma cools and solidifies, minerals within the magma begin to form crystals. The arrangement of atoms within these crystals gives the rock its characteristic appearance and properties. The crystals can range in size from tiny grain-like structures to large formations visible to the naked eye. Crystallization is an important part of the rock cycle as it creates new rocks from molten material, which can then be weathered and eroded to form sedimentary rocks or transformed through heat and pressure into metamorphic rocks.
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