Rock Identifier
Quartz (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: White to colorless, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: White to colorless, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed through the cooling and crystallization of magma or from hydrothermal veins. It is found in all geological environments and can be any age from Precambrian to modern.

Uses & applications

Used in glassmaking, abrasives, electronics (piezoelectric crystals), countertops, and jewelry/ornamental décor.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both chemical and physical weathering.

Field identification & locations

Identify in the field by its hardness (scratches glass), lack of cleavage, and glassy appearance. Found globally in mountains, riverbeds, and sands.