
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Pale yellowish-brown to grayish-brown; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Pale yellowish-brown to grayish-brown
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale yellowish-brown to grayish-brown; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed in igneous or metamorphic environments, primarily within hydrothermal veins or pegmatites. The smoky color results from natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used widely in lapidary work for jewelry, as ornamental interior design pieces, and as a popular specimen for mineral collectors. In industry, high-purity quartz is used in electronics and glass-making.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm'. The dark color can often be removed or lightened by heating the specimen.
Field identification & locations
Identify by its characteristic glassy luster and ability to scratch glass. It often shows internal fractures or phantoms. Commonly found in mountainous regions globally, such as the Alps, Brazil, and the USA.
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sedimentary
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Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic