
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Grayish-brown to black; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Grayish-brown to black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Grayish-brown 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 and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used primarily as a gemstone in jewelry, decorative ornaments, and as a popular specimen for mineral collectors. Some industrial use in electronics, though synthetic quartz is more common.
Geological facts
Smoky quartz gets its dark color from exposure to natural radiation from surrounding radioactive elements like uranium or thorium. Crystals can range from almost transparent to completely opaque black.
Field identification & locations
Identify by its characteristic 'smoky' translucency and 7 Mohs hardness (scratches glass). Commonly found in the Swiss Alps, Brazil, and Pikes Peak, Colorado. To field identify, look for hexagonal crystal faces and smoky coloration that does not rub off.
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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