
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Grayish-brown to black
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in igneous and metamorphic rocks, specifically in pegmatites and hydrothermal veins. The smoky color is caused by natural radiation from surrounding rocks acting on aluminum impurities within the quartz crystal.
Uses & applications
Used in jewelry as a gemstone, in crystal healing practices, and as decorative carvings or specimens for collectors. In industry, quartz is used for its piezoelectric properties and in glass making.
Geological facts
The dark color of smoky quartz can often be reversed by heating the specimen. It is the national gem of Scotland, where it is known as Cairngorm.
Field identification & locations
Identify in the field by its hardness (will scratch glass), conchoidal fracture, and characteristic smoky translucency. Found globally, with major deposits in Brazil, Madagascar, 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