
mineral
Diamond (or Cubic Zirconia)
C (Carbon) or ZrO2 (Zirconium Dioxide)
AI-generated identification · may be incorrectHardness: 10 (Diamond) or 8.0-8.5 (CZ); Color: Colorless; Luster: Adamantine; Crystal Structure: Isometric; Cleavage: Perfect octahedral (Diamond) or None (CZ); Specific Gravity: 3.52 (Diamond) or 5.6-6.0 (CZ)
- Hardness
- 10 (Diamond) or 8
- Color
- Colorless
- Luster
- Adamantine
Identified More mineral →
Explore Diamond (or Cubic Zirconia) in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 10 (Diamond) or 8.0-8.5 (CZ); Color: Colorless; Luster: Adamantine; Crystal Structure: Isometric; Cleavage: Perfect octahedral (Diamond) or None (CZ); Specific Gravity: 3.52 (Diamond) or 5.6-6.0 (CZ)
Formation & geological history
Natural diamonds form deep within the Earth's mantle under extreme pressure and heat, then are brought to the surface by kimberlite eruptions. Cubic Zirconia is typically lab-grown at temperatures around 4,982°F.
Uses & applications
Primarily used in high-end jewelry, industrial cutting tools, abrasives, and precision optics.
Geological facts
Diamond is the hardest natural substance on Earth. Cubic zirconia was developed as a cheaper, more durable alternative to diamonds for the jewelry market in the 1970s.
Field identification & locations
Identify by testing thermal conductivity or using a jeweler's loupe to look for inclusions; natural diamonds often have tiny flaws while CZ is perfectly clear. Found in kimberlite pipes or lab environments.
More like this
Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous