
mineral
Smoky Quartz
Silicon Dioxide (SiO2) with natural radiation induced color centers
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Grayish-brown to black; Luster: Vitreous; Crystal System: Trigonal (Hexagonal prisms); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Grayish-brown to black
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Grayish-brown to black; Luster: Vitreous; Crystal System: Trigonal (Hexagonal prisms); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous or metamorphic rocks through the cooling of silica-rich solutions in veins or pockets. Its color results from natural gamma radiation and small amounts of aluminum impurities within the crystal lattice.
Uses & applications
Used primarily in jewelry as a gemstone, decorative carvings, and in metaphysical collecting. Industrially, quartz is used in oscillators for watches and electronics.
Geological facts
Smoky Quartz is the national gem of Scotland, where it is known as Cairngorm. Large crystals weighing hundreds of pounds have been found in Brazil.
Field identification & locations
Identify by its hardness (scratches glass), lack of cleavage, and translucent brown/gray smoky color. Commonly found in pegmatite dikes and granite pockets within mountain ranges like the Alps or the Rockies.
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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