
mineral
Rough Diamond
Diamond (pure carbon / C)
AI-generated identification · may be incorrectHardness: 10 (Mohs scale); Color: Grayish-clear/translucent; Luster: Adamantine (greasy in rough state); Crystal structure: Isometric-hexoctahedral; Cleavage: Perfect in four directions; Specific Gravity: 3.5–3.53.
- Hardness
- 10 (Mohs scale)
- Color
- Grayish-clear/translucent
- Luster
- Adamantine (greasy in rough state)
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Physical properties
Hardness: 10 (Mohs scale); Color: Grayish-clear/translucent; Luster: Adamantine (greasy in rough state); Crystal structure: Isometric-hexoctahedral; Cleavage: Perfect in four directions; Specific Gravity: 3.5–3.53.
Formation & geological history
Formed under extreme pressure and high temperature (deep mantle, 150-250km deep) roughly 1 to 3.5 billion years ago. Brought to the surface via kimberlite or lamproite volcanic eruptions.
Uses & applications
Primary use in high-end jewelry (when cut/polished); significant industrial uses in cutting, drilling, and grinding tools due to extreme hardness.
Geological facts
Diamonds are the hardest known natural substance. The specimen in the image appears to be a 'maccle' or a rough industrial-grade diamond, showing the characteristic waxy/greasy luster and octahedral-like shape common in uncut stones.
Field identification & locations
Identify in the field by its high specific gravity (feels heavy for its size), greasy surface luster, and ability to scratch any other mineral. Commonly found in kimberlite pipes or alluvial deposits in Africa, Russia, and Canada.
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