
mineral
Smoky Quartz (Tumbled)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: translucent grayish-brown; Luster: vitreous (glassy); Crystal structure: Hexagonal (trigonal); Cleavage: none (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- translucent grayish-brown
- Luster
- vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: translucent grayish-brown; Luster: vitreous (glassy); Crystal structure: Hexagonal (trigonal); Cleavage: none (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed 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.
Uses & applications
Used in jewelry, decorative carvings, lapidary arts, and electronic components for its piezoelectric properties. It is also highly popular among mineral collectors.
Geological facts
Smoky quartz is the national gem of Scotland, where it is known as 'Cairngorm'. In ancient China, thin slices of smoky quartz were used to make the world's first sunglasses to protect the eyes from glare.
Field identification & locations
Identify by its translucent brown-to-black color and ability to scratch glass. Found globally, with notable deposits in Brazil, Switzerland, and the United States (Colorado). Field identification relies on hardness and lacks of cleavage.
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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