
mineral
Smoky Quartz
Silicon Dioxide (SiO2)
Mohs hardness of 7, vitreous luster, hexagonal crystal system (trigonal). Usually translucent to opaque with a smoky brown to grey color. White streak and conchoidal fracture.
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Physical properties
Mohs hardness of 7, vitreous luster, hexagonal crystal system (trigonal). Usually translucent to opaque with a smoky brown to grey color. White streak and conchoidal fracture.
Formation & geological history
Forms in intrusive igneous rocks (pegmatites) and metamorphic rocks. The smoky color is caused by natural gamma irradiation of the trace aluminum within the crystal lattice over millions of years.
Uses & applications
Used extensively in jewelry, ornamental carvings, and by collectors. In industry, quartz is used in glassmaking and electronics (piezoelectric properties), though smoky varieties are usually reserved for aesthetics.
Geological facts
Smoky Quartz was one of the first materials used for sunglasses in 12th century China to hide the expressions of judges in court. It is the national gem of Scotland, where it is known as Cairngorm.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and translucent 'smoky' appearance. Commonly found in Brazil, Madagascar, and the Swiss Alps.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic