Rock Identifier
Clear faceted gemstone, likely quartz (rock crystal) (Quartz, silicon dioxide (SiO₂); visual identification is uncertain because the stone is heavily faceted and photographed with flash) — gemstone
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Clear faceted gemstone, likely quartz (rock crystal)

Quartz, silicon dioxide (SiO₂); visual identification is uncertain because the stone is heavily faceted and photographed with flash

AI-generated identification · may be incorrect

Colorless and transparent with vitreous luster and numerous brilliant-cut facets; quartz has Mohs hardness 7, hexagonal crystal structure, no true cleavage, conchoidal fracture, and specific gravity about 2.65.…

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Physical properties

Colorless and transparent with vitreous luster and numerous brilliant-cut facets; quartz has Mohs hardness 7, hexagonal crystal structure, no true cleavage, conchoidal fracture, and specific gravity about 2.65. It could alternatively be glass or synthetic cubic zirconia, which cannot be reliably distinguished from this image.

Formation & geological history

Natural quartz forms in hydrothermal veins and igneous cavities, commonly from Paleozoic to younger geological settings; faceting is human processing. A gemstone identity requires hardness, refractive-index, and inclusion testing.

Uses & applications

Faceted quartz is used in inexpensive jewelry and ornaments; gem-quality quartz is collectible but generally modestly priced. If synthetic cubic zirconia, it is a diamond simulant rather than a natural mineral specimen.

Geological facts

Quartz commonly shows internal veils, fractures, or mineral inclusions; cubic zirconia is typically exceptionally bright and heavier. A loupe and polariscope can help, while a gem refractometer provides a strong separation.

Field identification & locations

Common sources include Brazil, Madagascar, the United States, and worldwide hydrothermal deposits. Test cautiously with a professional: glass scratches around Mohs 5–5.5, quartz scratches glass, and cubic zirconia has SG near 5.6.