
mineral
Smoky Quartz
Silicon Dioxide (SiO₂)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Brown, grey, to black; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Brown, grey, to black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Brown, grey, to black; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous and metamorphic rocks, particularly granite and pegmatite. The smoky color is caused by natural irradiation of aluminum-bearing quartz over millions of years within the Earth's crust.
Uses & applications
Used primarily in jewelry, ornamental carvings, and by crystal collectors. Historically used in China for early sunglasses and in electronics as a piezoelectric material.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm' because it is found in the Cairngorm Mountains. Extremely dark, opaque specimens are often called 'Morion'.
Field identification & locations
Identify in the field by its glassy luster, lack of cleavage, and its ability to scratch glass. It is commonly found in mountain ranges worldwide, particularly in Brazil, the Swiss Alps, and the United States (Colorado and Maine).
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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