
mineral
Smoky Quartz
Quartz (Silicon Dioxide) - SiO2
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Grayish-brown to black
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Grayish-brown to black; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed through the natural irradiation of aluminum-bearing clear quartz within granite pegmatites or hydrothermal veins. This specimen appears to have been extracted from a crystalline vein.
Uses & applications
Used in jewelry as gemstones, ornamental carvings, and widely collected by mineral enthusiasts. High-purity quartz is also used in electronics and glass manufacturing.
Geological facts
The dark color is caused by free silicon formed from the silicon dioxide by natural irradiation. If heated significantly, smoky quartz can lose its dark color and become clear or yellow.
Field identification & locations
Identify by its translucent smoky color, hexagonal crystal habits (if present), and its ability to scratch glass but not be scratched by a steel file. Commonly found in mountainous granitic regions.
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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