
mineral
Smoky Quartz
Silicon Dioxide (SiO2) with aluminum impurities
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent grey to brownish-black. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Translucent grey to brownish-black
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent grey to brownish-black. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in igneous and metamorphic rocks, particularly pegmatites and hydrothermal veins. The color comes from natural gamma radiation that activates aluminum impurities within the quartz lattice.
Uses & applications
Commonly used in jewelry (facets and beads), metaphysical practices, and as decorative collector specimens.
Geological facts
Unlike many dark minerals, smoky quartz remains translucent even in deep shades. It is the national gem of Scotland, where it is known as Cairngorm.
Field identification & locations
Identified by its transparency and distinct smoky grey-brown color. Found globally in granitic terrains. Collectors look for clarity and well-defined crystal terminations.
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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