Rock Identifier
Polished smoky quartz (likely iron-stained quartz) (Quartz, silicon dioxide (SiO₂); brown coloration may result from irradiation or iron-related staining/inclusions) — mineral
mineral

Polished smoky quartz (likely iron-stained quartz)

Quartz, silicon dioxide (SiO₂); brown coloration may result from irradiation or iron-related staining/inclusions

AI-generated identification · may be incorrect

Hardness 7 Mohs; translucent brown to smoky-black color, vitreous luster, conchoidal fracture, hexagonal crystal structure, and no cleavage. The glossy surface indicates polishing or tumbling.

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Physical properties

Hardness 7 Mohs; translucent brown to smoky-black color, vitreous luster, conchoidal fracture, hexagonal crystal structure, and no cleavage. The glossy surface indicates polishing or tumbling.

Formation & geological history

Quartz forms in hydrothermal veins, pegmatites, and cavities in igneous and metamorphic rocks; specimens may range from Precambrian to modern. Brown-red tones can reflect iron oxides or internal inclusions.

Uses & applications

Used as an ornamental and lapidary stone, carving material, and inexpensive jewelry or collector specimen; not typically used as aggregate in this polished form.

Geological facts

Quartz is one of Earth’s most abundant minerals and is chemically identical to clear rock crystal. Strongly transparent brown material is often sold as smoky quartz, while opaque iron-stained pieces may be marketed as brown quartz.

Field identification & locations

Identify by its glassy luster, hardness, lack of cleavage, and inability to scratch it with a steel knife; glass should not scratch it. Common sources include Brazil, Madagascar, the United States, Switzerland, and Spain.