
mineral
Diamond
Native Carbon (C)
AI-generated identification · may be incorrectHardness: 10 (Mohs scale); Color: Colorless (purest), yellow, brown, blue, green; Luster: Adamantine; Crystal structure: Isometric-Hexoctahedral; Cleavage: Perfect in four directions; Specific gravity: 3.52
- Hardness
- 10 (Mohs scale)
- Color
- Colorless (purest), yellow, brown, blue, green
- Luster
- Adamantine
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Physical properties
Hardness: 10 (Mohs scale); Color: Colorless (purest), yellow, brown, blue, green; Luster: Adamantine; Crystal structure: Isometric-Hexoctahedral; Cleavage: Perfect in four directions; Specific gravity: 3.52
Formation & geological history
Formed under high-pressure, high-temperature conditions deep within the Earth's mantle (140-190 km). Delivered to the surface through deep-origin volcanic eruptions known as kimberlite or lamproite pipes.
Uses & applications
Primary use in jewelry as a gemstone due to high dispersion and brilliance. Industrial uses include abrasives, cutting tools, drill bits, and heat sinks in high-end electronics.
Geological facts
Diamonds are the hardest known natural material. Most natural diamonds are between 1 billion and 3.5 billion years old. Famous specimens include the Hope Diamond and the Cullinan Diamond.
Field identification & locations
Identify by testing hardness (scratches all other materials), high thermal conductivity, and the presence of 'fire' (dispersion) in cut specimens. Found in primary deposits like kimberlite pipes or secondary alluvial deposits in riverbeds. Collectors look for clarity, color, and carat weight.
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