
mineral
Smoky Quartz
Smoky Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Grayish-brown to black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on 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 or metamorphic environments, particularly pegmatites. The smoky color is caused by natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used in gemstone jewelry, ornamental carvings, and as a popular specimen for mineral collectors. Historically used for ancient Chinese sunglasses.
Geological facts
Smoky quartz can range from nearly transparent to complete opacity. The dark black variety is known as 'Morion'. It is the national gem of Scotland, where it is often called 'Cairngorm'.
Field identification & locations
Identify by its glassy luster, lack of cleavage, and ability to scratch glass. Commonly found in granite mountains and vugs. Collectors should look for distinct crystal faces or the characteristic smoky translucence.
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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