
mineral
Diamond
Native Carbon (C)
AI-generated identification · may be incorrectHardness: 10 (Mohs scale); Color: Colorless (in this specimen), can range through all colors; Luster: Adamantine; Crystal Structure: Isometric (cubic); Cleavage: Perfect in four directions (octahedral); Specific Gravity: 3.52
- Hardness
- 10 (Mohs scale)
- Color
- Colorless (in this specimen), can range through all colors
- Luster
- Adamantine
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Physical properties
Hardness: 10 (Mohs scale); Color: Colorless (in this specimen), can range through all colors; Luster: Adamantine; Crystal Structure: Isometric (cubic); Cleavage: Perfect in four directions (octahedral); Specific Gravity: 3.52
Formation & geological history
Formed under extreme high pressure and temperature conditions deep within the Earth's mantle, approximately 100 miles below the surface, usually billions of years ago. Transported to the surface by kimberlite and lamproite pipes.
Uses & applications
Predominantly used in jewelry as a gemstone and in industry for cutting, grinding, and drilling tools due to its extreme hardness.
Geological facts
Diamond is the hardest naturally occurring substance on Earth. It is composed of a single element (carbon) arranged in an extremely strong tetrahedral structure. Many diamonds found today are 1 to 3 billion years old.
Field identification & locations
Identify by its brilliance, ability to scratch any other material, and high thermal conductivity. Commonly found in alluvial deposits or within kimberlite pipes in regions like South Africa, Russia, Canada, and Australia.
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