
mineral
Smoky quartz (possibly smoky quartz/chalcedony)
Quartz, silicon dioxide (SiO₂), likely natural smoky quartz with conchoidal fracture
AI-generated identification · may be incorrectHardness 7 Mohs; translucent gray-brown to smoky purple, vitreous luster, and no obvious cleavage. Quartz is trigonal and has a specific gravity near 2.65; the rough edges and conchoidal fractures are consistent with quartz.
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Physical properties
Hardness 7 Mohs; translucent gray-brown to smoky purple, vitreous luster, and no obvious cleavage. Quartz is trigonal and has a specific gravity near 2.65; the rough edges and conchoidal fractures are consistent with quartz.
Formation & geological history
Smoky color generally forms when natural radiation activates aluminum impurities in quartz, commonly in granitic pegmatites, hydrothermal veins, and alpine cavities. Crystals may range from ancient geological settings to relatively young vein deposits.
Uses & applications
Used as a collectible mineral and occasionally in cabochons or jewelry; quartz is also important industrially in glass, electronics, abrasives, and engineered stone.
Geological facts
The specimen may alternatively be dark chalcedony or agate, which is also microcrystalline quartz; a polished surface or testing is needed for certainty. Genuine smoky quartz can fade with strong heating or sunlight.
Field identification & locations
Look for glassy luster, conchoidal fracture, translucency, and scratch resistance greater than ordinary steel; it should scratch glass but not be scratched by a steel knife. Common sources include Brazil, Madagascar, Switzerland, the United States, 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
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary