Rock Identifier
Likely polished quartz or glass-like mineral cabochon (Probably quartz (SiO₂), though the image cannot exclude man-made glass) — mineral
mineral

Likely polished quartz or glass-like mineral cabochon

Probably quartz (SiO₂), though the image cannot exclude man-made glass

AI-generated identification · may be incorrect

Rounded, highly polished, transparent-to-translucent gray-brown piece with reflective internal surfaces; quartz has Mohs hardness 7, vitreous luster, hexagonal crystal structure, and no cleavage. The strongly domed, uniform appearance may also indicate glass or a resin-mounted specimen.

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Physical properties

Rounded, highly polished, transparent-to-translucent gray-brown piece with reflective internal surfaces; quartz has Mohs hardness 7, vitreous luster, hexagonal crystal structure, and no cleavage. The strongly domed, uniform appearance may also indicate glass or a resin-mounted specimen.

Formation & geological history

If quartz, it formed from silica-rich hydrothermal fluids or igneous processes, commonly during veins and pegmatites; its geological age depends on the host deposit. Polishing and shaping are human processing.

Uses & applications

Used as a cabochon, ornamental stone, jewelry component, or study specimen; quartz is also important in glass, electronics, and engineered materials.

Geological facts

The photograph alone is insufficient for confident mineral identification because the object is cut and polished and lacks visible crystal faces. A scratch test, specific gravity, and close inspection for bubbles would help distinguish quartz from glass.

Field identification & locations

Common quartz occurs worldwide, including Brazil, Madagascar, the United States, and many pegmatite regions. Quartz will not be scratched by a steel knife, whereas ordinary glass is typically softer; visible round bubbles strongly suggest glass.