
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; 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: Indistinct; Specific Gravity: 2.65
Formation & geological history
Formed in igneous and metamorphic rocks, especially pegmatites and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum impurities within the crystal structure.
Uses & applications
Used in jewelry (gemstones), electronics (piezoelectric applications), and is highly valued by mineral collectors for its metaphysical properties and aesthetic appeal.
Geological facts
Cairngorm is a famous variety of smoky quartz found in the Cairngorm Mountains of Scotland. It is the national gemstone of Scotland and has been used for centuries in Highland traditional dress.
Field identification & locations
Identify by its smoky transparency and crystal habit. It is often found in mountainous regions such as the Swiss Alps, Brazil, and the United States (Colorado). Collectors look for well-defined terminations and deep, uniform color.
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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