Rock Identifier
Quartz (Smoky/Clear variety) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Smoky/Clear variety)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Transparent to translucent greyish-white, 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: Transparent to translucent greyish-white, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed from silicon-rich hydrothermal veins or through the cooling of silica-saturated magma in igneous rocks; widely found across all geological ages in continental crust.

Uses & applications

Used in glass making, electronics (piezoelectric properties), abrasives, as a semi-precious gemstone in jewelry, and highly popular for mineral collectors.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which has Slavic origins meaning 'hard'. It is highly resistant to chemical and physical weathering.

Field identification & locations

Identified in the field by its hardness (scratches glass), lack of cleavage, and glassy appearance. It is commonly found in riverbeds, mountains, and as a component of granite.