
mineral
Diamond
Diamond (C)
Hardness: 10 (Mohs scale), Color: Colorless to faint yellow/brown (jewelry grade), Luster: Adamantine, Crystal Structure: Isometric-Hexoctahedral, Cleavage: Perfect in four directions (octahedral), Specific Gravity: 3.52
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Physical properties
Hardness: 10 (Mohs scale), Color: Colorless to faint yellow/brown (jewelry grade), Luster: Adamantine, Crystal Structure: Isometric-Hexoctahedral, Cleavage: Perfect in four directions (octahedral), Specific Gravity: 3.52
Formation & geological history
Formed under high-pressure, high-temperature conditions in the Earth's mantle, approximately 100 miles below the surface, and brought upward by deep-source volcanic eruptions called kimberlite pipes. Most natural diamonds are between 1 billion and 3.5 billion years old.
Uses & applications
Primarily used in jewelry; industrial use as abrasives and for cutting/drilling tools due to extreme hardness.
Geological facts
Diamonds are the hardest known natural material on Earth and are composed of pure carbon arranged in a crystal lattice. The word 'diamond' comes from the ancient Greek 'adamas', meaning unbreakable.
Field identification & locations
Identify in jewelry by high dispersion (fire), extreme hardness, and metal settings. In nature, they are often found in kimberlite or lamproite rocks or secondary alluvial deposits. For collectors, look for the 'Four Cs': Cut, Color, Clarity, and Carat weight.
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