
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Brown to black, smoky gray; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Brown to black, smoky gray
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Brown to black, smoky gray; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
Formation & geological history
Formed in igneous and metamorphic rocks, particularly granite pegmatites and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum-containing quartz during geological timescales.
Uses & applications
Commonly used in jewelry (faceting and cabochons), metaphysical practices, and as a popular collector specimen. Industrially, quartz is used in glassmaking and electronics.
Geological facts
The dark brown to black varieties are often called 'Cairngorm' in Scotland. Very dark, opaque smoky quartz is known as 'Morion.' It is the national gem of Scotland.
Field identification & locations
Identify by its characteristic glassy luster and smoky transparency. It will scratch glass but cannot be scratched by a steel knife. Commonly found in Brazil, USA (Colorado), 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