
mineral
Smoky Quartz
Smoky Quartz (Silicon Dioxide - SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Brownish-grey, black, or smoky translucent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Brownish-grey, black, or smoky translucent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Brownish-grey, black, or smoky translucent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in igneous or metamorphic rocks like granite or gneiss. It acquires its smoky color through natural irradiation of trace aluminum impurities over millions of years.
Uses & applications
Used in gemstone jewelry, ornamental carvings, and historical optical instruments. It is also a very popular specimen for mineral collectors.
Geological facts
Smoky quartz is the national gem of Scotland, where it is often referred to as 'Cairngorm'. Its dark color is a result of free silicon, formed from the silicon dioxide by natural radiation.
Field identification & locations
Identify by its translucent brownish tint and glassy fracture surfaces. It is typically found in pegmatite dikes and alpine-type fissures globally, especially in Brazil and the USA.
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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