Rock Identifier
Polished smoky quartz crystal with inclusions (Quartz, silicon dioxide (SiO₂), likely smoky quartz with iron-oxide or other mineral inclusions) — mineral
mineral

Polished smoky quartz crystal with inclusions

Quartz, silicon dioxide (SiO₂), likely smoky quartz with iron-oxide or other mineral inclusions

AI-generated identification · may be incorrect

Mohs hardness 7; translucent gray-brown to nearly clear, with vitreous luster and conchoidal fracture. Hexagonal quartz structure; the apparent flat base and pointed top indicate it was cut or shaped rather than naturally terminated.

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Physical properties

Mohs hardness 7; translucent gray-brown to nearly clear, with vitreous luster and conchoidal fracture. Hexagonal quartz structure; the apparent flat base and pointed top indicate it was cut or shaped rather than naturally terminated.

Formation & geological history

Quartz crystallizes from silica-rich hydrothermal fluids in cavities of igneous and metamorphic rocks, commonly during the Paleozoic–Cenozoic; exact age cannot be determined from the image.

Uses & applications

Used as a collector specimen, ornamental stone, and occasionally in jewelry; included quartz is generally more decorative than gem-grade.

Geological facts

The dark smoky color commonly results from radiation-induced color centers associated with aluminum impurities; heating can partially remove the color.

Field identification & locations

Identify by its glassy luster, hardness, lack of obvious cleavage, and hexagonal crystal habit; common sources include Brazil, Madagascar, Switzerland, and the United States. The inclusions may also indicate tourmaline, mica, or iron oxides, but visual confirmation is insufficient.