
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent smoky grey to brownish-black; Luster: Vitreous; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent smoky grey to brownish-black
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent smoky grey to brownish-black; Luster: Vitreous; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed in igneous and metamorphic rocks, particularly granite pegmatites. The smoky color is caused by natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used extensively in jewelry (as gemstones), decorative carvings, and as a popular specimen for mineral collectors. Some industrial use in electronics, though synthetic quartz is more common there.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm'. In ancient China, it was used to create the first sunglasses to hide the wearer's facial expressions in court.
Field identification & locations
Identified by its distinctive smoky translucency and hardness (it will scratch glass). It is commonly found in mountain ranges such as the Alps, Brazil, and the United States (Colorado).
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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