
mineral
Diamond (in a gold setting)
Carbon (C)
Hardness: 10 (Mohs scale), Color: Colorless (in this specimen), Luster: Adamantine, Crystal Structure: Isometric-hexoctahedral, Cleavage: Octahedral, Specific Gravity: 3.52
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Physical properties
Hardness: 10 (Mohs scale), Color: Colorless (in this specimen), Luster: Adamantine, Crystal Structure: Isometric-hexoctahedral, Cleavage: Octahedral, Specific Gravity: 3.52
Formation & geological history
Formed under high-pressure, high-temperature conditions in Earth's mantle, typically at depths of 140 to 190 kilometers. They are brought to the surface through volcanic eruptions known as kimberlites.
Uses & applications
Used primarily in fine jewelry (engagement rings, necklaces) and extensively in industry for cutting, drilling, and grinding due to its extreme hardness.
Geological facts
Diamonds are the hardest known natural material on Earth. Most natural diamonds have ages between 1 billion and 3.5 billion years.
Field identification & locations
Identified by its high refractive index, extreme hardness, and specific thermal conductivity. Look for a 'hallmark' on the inside of the ring band to identify metal purity (e.g., 14k, 18k).
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mineral