Rock Identifier
Smoky Quartz (Silicon Dioxide (SiO2) with aluminum impurities) — mineral
mineral

Smoky Quartz

Silicon Dioxide (SiO2) with aluminum impurities

Hardness: 7.0 Mohs. Color: Translucent to opaque brown-gray to black. Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: Indistinct. Specific Gravity: 2.65.

Hardness
7
Color
Translucent to opaque brown-gray to black
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7.0 Mohs. Color: Translucent to opaque brown-gray to black. Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: Indistinct. Specific Gravity: 2.65.

Formation & geological history

Formed in igneous rocks like granite and pegmatites through the natural irradiation of aluminum-bearing quartz over millions of years. It occurs in hydrothermal veins and metamorphic rocks as well.

Uses & applications

Used widely in lapidary for jewelry, ornamental carvings, and decorative crystals. Historically used for making the first sunglasses in 12th century China.

Geological facts

The dark color is caused by free silicon formed from silicon dioxide by natural irradiation of the crystal at the time of its growth or later. Cairngorm is a popular name for smoky quartz found in the Cairngorm Mountains of Scotland.

Field identification & locations

Identify by its smoky-brown color, transparency, and hardness (it will scratch glass but not a steel file). It is commonly found in Brazil, Madagascar, the Swiss Alps, and the Pikes Peak area of Colorado.