Rock Identifier
Smoky quartz (Quartz (silicon dioxide, SiO₂), likely a rough smoky-quartz fragment) — mineral
mineral

Smoky quartz

Quartz (silicon dioxide, SiO₂), likely a rough smoky-quartz fragment

AI-generated identification · may be incorrect

Mohs hardness 7; translucent gray-brown to pale smoky color, vitreous luster, trigonal crystal structure, and no cleavage; typically breaks with conchoidal fracture. The image shows a rough, partly translucent fragment, though color alone is not diagnostic.

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Physical properties

Mohs hardness 7; translucent gray-brown to pale smoky color, vitreous luster, trigonal crystal structure, and no cleavage; typically breaks with conchoidal fracture. The image shows a rough, partly translucent fragment, though color alone is not diagnostic.

Formation & geological history

Forms in silica-rich veins and cavities, commonly in granitic pegmatites and hydrothermal environments; its smoky color develops from irradiation affecting trace aluminum in the crystal. Quartz occurs in rocks of many geological ages.

Uses & applications

Used in jewelry and ornamental carvings; quartz is also important in glassmaking, electronics, and industrial applications.

Geological facts

Quartz is among Earth’s most abundant minerals; smoky coloration can range from nearly clear to very dark brown.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch ordinary glass, and lack of cleavage. Common sources include Brazil, Madagascar, the Alps, and the western United States.