
mineral
Smoky Quartz (Tumbled)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent brownish-grey to smoky yellow; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Translucent brownish-grey to smoky yellow
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent brownish-grey to smoky yellow; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the igneous process in granite pegmatites or hydrothermal veins. The smoky color is caused by natural irradiation of aluminum-containing rock crystal during its geological history, often spanning millions of years.
Uses & applications
Commonly used in jewelry as a gemstone, as well as in the production of quartz watches, piezoelectric devices, and by collectors for its aesthetic and 'grounding' metaphysical properties.
Geological facts
Smoky Quartz is the national gem of Scotland, where it is known as 'Cairngorm.' It was used in Ancient China to make the first-ever sunglasses to conceal the facial expressions of judges in courts.
Field identification & locations
Identify by its characteristic 'smoky' translucency and hardness (it will scratch glass). Commonly found in the Swiss Alps, Brazil, Madagascar, and the United States (Colorado). Field identification relies on the lack of cleavage and its smoke-like inclusions.
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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