
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs; Color: Brownish-grey to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
- Hardness
- 7 Mohs
- Color
- Brownish-grey to black
- Luster
- Vitreous
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Physical properties
Hardness: 7 Mohs; Color: Brownish-grey to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
Formation & geological history
Forms in intrusive igneous and metamorphic rocks, particularly pegmatites. The color is produced by natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used extensively in jewelry as a gemstone, in ornamental carvings, and by crystal collectors. Historically used for making early sunglasses in China.
Geological facts
The dark color of Smoky Quartz is caused when silicon dioxide is exposed to natural radiation from surrounding radioactive elements like uranium or thorium in the host rock.
Field identification & locations
Identify by its translucent brownish color and glassy luster. It can be found globally, with major deposits in Brazil, Madagascar, 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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary