
mineral
Tumbled smoky quartz
Quartz (silicon dioxide, SiO₂), smoky variety
AI-generated identification · may be incorrectHardness 7 Mohs; translucent smoky brown to nearly black, with vitreous luster and conchoidal fracture. The rounded shape is mechanically polished; internal veils and fractures are visible, while the bright cyan rim appears to be reflected light or surface coating.
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Physical properties
Hardness 7 Mohs; translucent smoky brown to nearly black, with vitreous luster and conchoidal fracture. The rounded shape is mechanically polished; internal veils and fractures are visible, while the bright cyan rim appears to be reflected light or surface coating.
Formation & geological history
Smoky quartz forms when natural irradiation creates color centers in quartz, commonly in granitic pegmatites and hydrothermal veins. It is generally associated with Paleozoic–Mesozoic and younger granitic systems, though the specimen’s age cannot be determined visually.
Uses & applications
Used as a decorative and lapidary stone, in carvings and inexpensive jewelry, and commonly sold as a tumbled healing or display stone.
Geological facts
Smoky quartz is colored by trace aluminum-related defects activated by radiation; heating can reduce or remove the smoky color. Very dark material may be marketed as morion.
Field identification & locations
Identify by its glassy luster, hardness, translucent brown color, and lack of obvious cleavage; it can scratch ordinary glass but not be scratched by steel easily. Common sources include Brazil, Switzerland, the United States, Madagascar, and Scotland.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
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