
mineral
Smoky Quartz
Smoky Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale; Color: Brownish-grey, black, or translucent smoke-color; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Brownish-grey, black, or translucent smoke-color
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Brownish-grey, black, or translucent smoke-color; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous or metamorphic rocks like granite or pegmatites. The smoky color is caused by natural gamma radiation from surrounding minerals that induces color centers in the quartz lattice around aluminum impurities.
Uses & applications
Used primarily in lapidary work for jewelry (beads, cabochons, faceted gems), ornamental carvings, and as a popular specimen for mineral collectors.
Geological facts
Smoky quartz is the national gem of Scotland, where it is often referred to as 'Cairngorm.' Some of the darkest varieties are called 'Morion.' It was used for sunglasses in 12th century China.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and translucent brown color. Commonly found in mountainous regions like the Alps, Brazil, and the United States (Colorado).
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