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Quartz is formed through a geological process involving the crystallization of silica (silicon dioxide) from molten magma or through the precipitation of minerals from aqueous solutions. Over time, silica-rich solutions fill cavities in rocks, and as the solution cools or evaporates, quartz crystals begin to form. These crystals grow in size through repeated cycles of crystallization, resulting in the clear, hard mineral known as quartz. Additionally, quartz can form in sedimentary environments through the accumulation and compaction of silica-rich sediments.

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1mo ago

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