
mineral
Smoky Quartz Cluster
Quartz (Silicon Dioxide) - SiO2
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Brown, black, or grey smoky hues; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Brown, black, or grey smoky hues
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Brown, black, or grey smoky hues; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed in pegmatites, hydrothermal veins, and igneous rocks through the natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used in gemstone carvings, jewelry, metaphysical collection, and historically in some optical components or early sunglasses in China.
Geological facts
The brown color is caused by free silicon formed from the silicon dioxide by natural irradiation. It is the national gem of Scotland, where it is often referred to as 'Cairngorm' after the mountain range.
Field identification & locations
Identify in the field by its crystal habit (six-sided prisms meeting at a point), its ability to scratch glass, and the lack of cleavage. Commonly found in granite-rich mountainous regions.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
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