
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale; Color: transluculent grey, brown, to nearly black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on the Mohs scale
- Color
- transluculent grey, brown, to nearly black
- Luster
- Vitreous
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Physical properties
Hardness: 7 on the Mohs scale; Color: transluculent grey, brown, to nearly black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in igneous and metamorphic rocks, particularly pegmatites and hydrothermal veins. The smoky color is caused by natural irradiation of aluminum impurities within the crystal lattice over millions of years.
Uses & applications
Used frequently in jewelry (faceted stones and beads), ornamental carvings, and by collectors. In industry, quartz is used in glass making and electronics, though high-clarity natural smoky quartz is more aesthetic in value.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm' after the mountain range where it was historically mined. It can vary from 'Morion' (nearly black) to 'Cairngorm' (yellow-brown).
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and smoky translucent color. It is commonly found in Brazil, Madagascar, the Swiss Alps, and the United States (Colorado and New Hampshire).
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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