
mineral
Smoky quartz
Quartz, silicon dioxide (SiO₂), brown to gray variety
AI-generated identification · may be incorrectHardness 7 Mohs; translucent smoky-brown to gray, vitreous luster, conchoidal fracture, no cleavage, hexagonal crystal structure. The specimen appears rough and partly weathered, with possible iron-oxide staining or matrix.
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Physical properties
Hardness 7 Mohs; translucent smoky-brown to gray, vitreous luster, conchoidal fracture, no cleavage, hexagonal crystal structure. The specimen appears rough and partly weathered, with possible iron-oxide staining or matrix.
Formation & geological history
Forms in silica-rich hydrothermal veins, pegmatites, and cavities of igneous rocks; smoky color commonly results from natural irradiation affecting aluminum impurities. Individual crystals may range from recent geologic growth to hundreds of millions of years old.
Uses & applications
Used as a collector mineral and occasionally in jewelry; quartz is also important in glassmaking, electronics, foundry applications, and engineered stone.
Geological facts
Smoky quartz is one of the most common quartz varieties and can be naturally darkened or artificially irradiated. Its conchoidal fracture and glassy appearance distinguish it from many dark rocks.
Field identification & locations
Common localities include Brazil, Switzerland, Scotland, the United States, Madagascar, and Spain. Confirm with a hardness test against glass and inspect for conchoidal fracture; avoid scratching valuable specimens.
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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