Inorganic Chemistry II
Quartz is a crystalline mineral composed of silicon dioxide (SiO₂), and it is one of the most abundant minerals found in the Earth's crust. Its well-defined crystal structure results in its characteristic hexagonal shape, and it exhibits a wide range of physical properties, including hardness and resistance to weathering. Quartz plays a significant role in the study of bonding in solids, particularly in understanding covalent bonding and the arrangement of atoms within solid structures.
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