Rock Identifier
Faceted colorless gemstone, likely quartz (rock crystal) or synthetic glass imitation (Quartz: silicon dioxide (SiO₂), trigonal crystal system; exact identity cannot be confirmed visually) — gemstone
gemstone

Faceted colorless gemstone, likely quartz (rock crystal) or synthetic glass imitation

Quartz: silicon dioxide (SiO₂), trigonal crystal system; exact identity cannot be confirmed visually

AI-generated identification · may be incorrect

Colorless, transparent, vitreous luster, faceted brilliant-style cut, and no visible natural crystal faces. Quartz hardness is Mohs 7, specific gravity 2.65, and lacks cleavage; glass is softer (about 5–5.5) and commonly shows bubbles or curved facet wear.

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Physical properties

Colorless, transparent, vitreous luster, faceted brilliant-style cut, and no visible natural crystal faces. Quartz hardness is Mohs 7, specific gravity 2.65, and lacks cleavage; glass is softer (about 5–5.5) and commonly shows bubbles or curved facet wear.

Formation & geological history

Natural quartz forms in hydrothermal veins and cavities, commonly from Paleozoic to younger geological settings. The pictured cut object may also be laboratory-grown quartz or lead-free glass, so age and formation cannot be established from the image.

Uses & applications

Used as a gemstone, ornament, and collector piece; quartz is also important in electronics and industry. Glass imitations have mainly decorative value.

Geological facts

A loupe, refractometer, polariscope, and hardness testing are needed for reliable identification. Faceting and the unusually large, highly uniform appearance suggest a cut specimen rather than a natural crystal.

Field identification & locations

Check for gas bubbles, curved facet edges, scratches, and double refraction; quartz can scratch glass, while ordinary glass generally cannot scratch quartz. Natural gem-quality quartz is common in Brazil, Madagascar, Arkansas, and the Alps.