Rock Identifier
Colorless faceted gemstone, likely synthetic cubic zirconia (Cubic zirconia (zirconium dioxide, ZrO₂); natural diamond is a less likely alternative) — gemstone
gemstone

Colorless faceted gemstone, likely synthetic cubic zirconia

Cubic zirconia (zirconium dioxide, ZrO₂); natural diamond is a less likely alternative

AI-generated identification · may be incorrect

Colorless, transparent, adamantine-to-glassy luster, and brilliant faceting. Cubic zirconia has Mohs hardness about 8–8.5 and cubic crystal structure; diamond is Mohs 10 with an adamantine luster and octahedral cleavage. The photograph cannot confirm identity or distinguish it reliably from glass.

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Physical properties

Colorless, transparent, adamantine-to-glassy luster, and brilliant faceting. Cubic zirconia has Mohs hardness about 8–8.5 and cubic crystal structure; diamond is Mohs 10 with an adamantine luster and octahedral cleavage. The photograph cannot confirm identity or distinguish it reliably from glass.

Formation & geological history

Cubic zirconia is laboratory-grown by melting zirconium oxide with stabilizers; it is not a natural rock. Natural diamond forms deep in Earth’s mantle under extreme pressure and temperature, commonly more than 1 billion years ago, then reaches the surface in kimberlite.

Uses & applications

Used as an inexpensive diamond simulant in jewelry and ornaments. Approximate value is $1–$30 for a loose common cubic-zirconia stone; a genuine diamond of similar appearance could range from hundreds to many thousands of dollars depending on carat weight and grading.

Geological facts

The large, intensely reflective appearance and visible facet pattern are consistent with a cut simulant, but image glare obscures inclusions and facet quality.

Field identification & locations

Check loupe magnification, refractive index, thermal conductivity, dispersion, and specific gravity; professional gemological testing is required. Cubic zirconia is commonly manufactured worldwide, while diamonds occur in kimberlite and alluvial deposits.