
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs; Color: Brownish-grey to black smoky translucence; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 Mohs
- Color
- Brownish-grey to black smoky translucence
- Luster
- Vitreous
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Physical properties
Hardness: 7 Mohs; Color: Brownish-grey to black smoky translucence; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous and metamorphic rocks, primarily pegmatites and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum-containing quartz over millions of years.
Uses & applications
Used extensively in jewelry as gemstones, in metaphysical practices, and as collector specimens. Occasionally used in industrial optics.
Geological facts
The dark color is often the result of free silicon formed from silicon dioxide by natural radiation. Rare, nearly opaque black varieties are known as 'Morion'.
Field identification & locations
Identified by its transparency, smoky brown hue, and hardness (scratches glass). Look for lack of cleavage and typical quartz hexagonal prism habits in raw forms. Found in Brazil, USA, and the Swiss Alps.
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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