
mineral
Smoky quartz (likely)
Quartz, silicon dioxide (SiO₂), naturally irradiated variety
AI-generated identification · may be incorrectDark smoky-brown to nearly black, translucent in thinner edges, with vitreous luster and conchoidal fracture; Mohs hardness 7, no cleavage, trigonal crystal structure. The rough form may show crystal faces or fracture surfaces.
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Physical properties
Dark smoky-brown to nearly black, translucent in thinner edges, with vitreous luster and conchoidal fracture; Mohs hardness 7, no cleavage, trigonal crystal structure. The rough form may show crystal faces or fracture surfaces.
Formation & geological history
Forms in silica-rich hydrothermal veins, pegmatites, and cavities in igneous rocks when trace aluminum is irradiated naturally, typically during late stages of granite formation. Individual crystals can range from geologically young to hundreds of millions of years old.
Uses & applications
Used as a collector mineral, ornamental stone, and occasionally in jewelry; darker transparent material is most desirable. Common rough pieces have modest commercial value.
Geological facts
Smoky quartz can be artificially irradiated or heat-treated, though natural color is common. Very dark material is sometimes called morion.
Field identification & locations
Common localities include Brazil, Switzerland, Scotland, Colorado, Arkansas, and Madagascar. Confirm with a glass-scratch test only cautiously: quartz should scratch ordinary glass, while its lack of cleavage distinguishes it from many dark minerals.
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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