
mineral
Diamond
Diamond (pure carbon, C)
Hardness: 10 (Mohs scale); Color: colorless (in this specimen), can be yellow, brown, or blue; Luster: Adamantine; Crystal Structure: Isometric-Hexoctahedral; Cleavage: 111 (perfect octahedral); Specific Gravity: 3.52
- Hardness
- 10 (Mohs scale)
- Color
- colorless (in this specimen), can be yellow, brown, or blue
- Luster
- Adamantine
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Physical properties
Hardness: 10 (Mohs scale); Color: colorless (in this specimen), can be yellow, brown, or blue; Luster: Adamantine; Crystal Structure: Isometric-Hexoctahedral; Cleavage: 111 (perfect octahedral); Specific Gravity: 3.52
Formation & geological history
Formed deep within the Earth's mantle (150-250 km deep) under extreme high pressure and temperature. Transported to the surface via volcanic eruptions in kimberlite or lamproite pipes. Most diamonds are 1 to 3.5 billion years old.
Uses & applications
Primary use in high-end jewelry (engagement rings, necklaces), and industrial applications including cutting, grinding, and drilling tools due to extreme hardness.
Geological facts
Diamond is the hardest natural substance on Earth. The name comes from the Greek word 'adamas', meaning unbreakable. Some diamonds are extraterrestrial, found in meteorites.
Field identification & locations
Identify by its extreme hardness (scratches all other minerals), high thermal conductivity, and characteristic 'brilliant' luster. Commonly found in secondary alluvial deposits or primary kimberlite pipes in regions like South Africa, Russia, and Canada.
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mineral