
mineral
Smoky Quartz (with inclusions)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Gray, brownish-black, translucent to semi-opaque; Luster: Vitreous to greasy on fracture surfaces; Crystal Structure: Trigonal (hexagonal prisms); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Gray, brownish-black, translucent to semi-opaque
- Luster
- Vitreous to greasy on fracture surfaces
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, brownish-black, translucent to semi-opaque; Luster: Vitreous to greasy on fracture surfaces; Crystal Structure: Trigonal (hexagonal prisms); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous and metamorphic environments, specifically pegmatites and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum-bearing quartz over millions of years.
Uses & applications
Used in gemstone jewelry, ornamental carvings, and as a popular specimen for mineral collectors. Some industrial uses include pressure sensors due to piezoelectric properties.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm.' The color can range from a light yellowish gray to a black so dark it is nearly opaque.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and characteristic smoky translucency. Commonly found in mountainous regions like 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
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)
igneous