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

Smoky Quartz

Quartz (Silicon Dioxide) - SiO2

Hardness: 7 on Mohs scale. Color: Smoky gray, brownish-gray, to translucent dark gray. Luster: Vitreous (glassy). Crystal Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Smoky gray, brownish-gray, to translucent dark gray
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale. Color: Smoky gray, brownish-gray, to translucent dark gray. Luster: Vitreous (glassy). Crystal Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Formed in pegmatites, granitic rocks, and hydrothermal veins. The distinct brownish-gray color is caused by natural irradiation of aluminum impurities within the crystal lattice.

Uses & applications

Popular among gem collectors, used in jewelry, cabochons, carved ornaments, and as ornamental display minerals.

Geological facts

Smoky quartz was historically used in China during the 12th century to make early sunglasses. It is also the national gem of Scotland, where it is known as Cairngorm.

Field identification & locations

Identified by its transparent to translucent smoky gray color and vitreous fracture. Commonly found in granitic pegmatites worldwide including Brazil, Madagascar, the US (Colorado), and the Swiss Alps.