
Mineral
Diamond
Diamond (C)
Hardness: 10 (Mohs scale), Color: Typically colorless, but can be yellow, brown, green, blue, pink, red, gray, or black due to impurities. Luster: Adamantine (brilliant, diamond-like). Crystal Structure: Isometric (cubic), commonly octahedral, dodecahedral, or cubic crystals. Cleavage: Perfect octahedral.…
- Luster
- Adamantine (brilliant, diamond-like)
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Physical properties
Hardness: 10 (Mohs scale), Color: Typically colorless, but can be yellow, brown, green, blue, pink, red, gray, or black due to impurities. Luster: Adamantine (brilliant, diamond-like). Crystal Structure: Isometric (cubic), commonly octahedral, dodecahedral, or cubic crystals. Cleavage: Perfect octahedral. Specific Gravity: 3.5-3.53.
Formation & geological history
Formation Process: Diamonds form under extremely high pressure and temperature conditions, typically within the Earth's mantle (about 150-200 km deep). They are brought to the surface through volcanic eruptions in kimberlite and lamproite pipes. Geological Age: Most natural diamonds are between 1 billion and 3.5 billion years old.
Uses & applications
Industry: Cutting, grinding, and drilling tools, abrasives, windows for vacuum systems, heat sinks for electronics. Jewelry: Highly valued as gemstones for rings, necklaces, and other adornments due to their brilliance and durability. Construction: Used in drill bits for tunneling and rock excavation (industrial diamonds).
Geological facts
Diamond is the hardest known natural material, making it an excellent abrasive. Its exceptional brilliance and fire make it highly prized as a gemstone. Diamonds are often dated by analyzing inclusions within them, such as tiny pockets of other minerals, providing clues about their geological age. The largest gem-quality diamond ever found is the Cullinan Diamond (3,106.75 carats).
Field identification & locations
Field Identification: Distinguished by its extreme hardness (scratches all other minerals), adamantine luster, and typical octahedral crystal habit (though often found as fragments). Can also be identified by its high thermal conductivity. Common Locations: Primarily found in kimberlite and lamproite pipes, which are ancient volcanic conduits. Major diamond producing countries include Russia, Botswana, Australia, Canada, South Africa, Angola, and the Democratic Republic of Congo. Tips for Collectors: Raw diamonds often appear as dull, greasy-looking crystals. Look for characteristic octahedral or dodecahedral shapes. Due to their high value, proper identification and verification are crucial.
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