
mineral
Smoky Quartz
SiO2 (Silicon Dioxide)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent gray to black; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent gray to black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent gray to black; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.
Formation & geological history
Formed in igneous and metamorphic rocks, particularly pegmatites. The smoky color is caused by natural irradiation of aluminum impurities within the crystal lattice during formation over millions of years.
Uses & applications
Used extensively in jewelry as a gemstone, in crystal healing practices, and as ornamental display specimens for collectors.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm'. Traditionally, it was used in early Chinese sunglasses in the 12th century.
Field identification & locations
Identify by its characteristic 'smoke' color and glass-like clarity. It is common in mountain ranges like the Alps, Brazil, and Madagascar. Collectors look for high transparency and well-defined crystal points.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous