Cubic Zirconia (Simulated Diamond)
Zirconium dioxide (ZrO2)
Rock Type: mineral

Physical Properties
Hardness: 8-8.5 Mohs scale. Color: Typically colorless but can be synthesized in many colors. Luster: Adamantine. Crystal structure: Isometric (cubic). Specific Gravity: 5.6-6.0 (much denser than diamond).
Formation & Geological History
While zirconium dioxide occurs naturally as the rare mineral baddeleyite, jewelry-grade cubic zirconia is a synthetic material grown in a laboratory using the 'skull melting' process. Commercial production began in the 1970s.
Uses & Applications
Primary use is as a low-cost diamond alternative in jewelry. Also used as a thermal insulator in industrial applications and in optical components.
Geological Facts
Cubic Zirconia is roughly 1.7 times heavier than a diamond of the same size. Unlike naturally occurring diamonds which often have inclusions, lab-grown CZ is usually entirely flawless.
Field Identification & Locations
Identify by weight (it will feel heavier than expected) and by its 'fire' (it has more rainbow light dispersion than a diamond). It will also show visible wear and scratches over time that a diamond would not.
Identified on: 4/26/2026
Mode: Standard