
mineral
Smoky quartz crystal/rough fragment
Quartz (SiO₂), likely smoky quartz
AI-generated identification · may be incorrectTypically Mohs hardness 7, vitreous luster, translucent gray-brown to smoky coloration, conchoidal fracture, and no cleavage; hexagonal crystal structure. The pictured piece appears irregular and partly crystalline, with possible surface weathering or matrix.
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Physical properties
Typically Mohs hardness 7, vitreous luster, translucent gray-brown to smoky coloration, conchoidal fracture, and no cleavage; hexagonal crystal structure. The pictured piece appears irregular and partly crystalline, with possible surface weathering or matrix.
Formation & geological history
Forms in silica-rich hydrothermal veins, cavities in igneous rocks, and pegmatites; smoky color commonly results from natural irradiation acting on aluminum impurities. Individual crystals may form over long spans of geologic time, from Precambrian to recent hydrothermal settings.
Uses & applications
Used for ornaments, carvings, crystal collecting, and occasionally jewelry; quartz is also important industrially in glass, electronics, abrasives, and engineered stone.
Geological facts
Smoky quartz is the brown variety of quartz; darker examples are sometimes called morion. Color can fade with prolonged heating or intense light.
Field identification & locations
Identify by hardness, glassy luster, lack of cleavage, and conchoidal fracture; it should scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Switzerland, Madagascar, the United States, and Scotland.
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Sandstone (with potential mineral staining/concretions)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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