
mineral
Diamond
Diamond (Carbon, C)
Hardness (Mohs scale): 10, the hardest known natural material. Color: Ranges from colorless to yellow, brown, gray, green, blue, pink, red, orange, and black, with colorless being the most prized. Luster: Adamantine (diamond-like), exceptionally brilliant.…
- Luster
- Adamantine (diamond-like), exceptionally brilliant
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Physical properties
Hardness (Mohs scale): 10, the hardest known natural material. Color: Ranges from colorless to yellow, brown, gray, green, blue, pink, red, orange, and black, with colorless being the most prized. Luster: Adamantine (diamond-like), exceptionally brilliant. Crystal Structure: Isometric (cubical), often found as octahedrons, dodecahedrons, or cubes. Cleavage: Perfect octahedral cleavage in four directions. Specific Gravity: 3.5-3.53.
Formation & geological history
Diamonds form in the Earth's mantle at depths of 150-200 km (90-120 miles) under immense pressure (45-60 kilobars) and high temperatures (900-1300°C). They are brought to the surface through deep-seated volcanic eruptions, forming kimberlite and lamproite pipes. Most exploitable diamond deposits are found in these igneous rock formations, or in secondary alluvial deposits where diamonds have been eroded from their primary sources and transported by water. Geological Age: Most natural diamonds are between 1 billion and 3.5 billion years old.
Uses & applications
Diamonds are highly valued for their beauty and durability. Primary uses include: Jewelry (gemstones): Cut and polished for rings, necklaces, earrings, and other ornaments due to their exceptional brilliance and fire. Industrial applications: Used in cutting, grinding, drilling, and polishing tools due to their extreme hardness. Examples include drill bits, saw blades, and abrasive powders. Scientific research: Used in high-pressure experiments due to their strength.
Geological facts
Diamonds are the hardest natural substance on Earth. They are formed under extremely high pressure and temperature conditions deep within the Earth's mantle. The word 'diamond' comes from the ancient Greek 'adamas', meaning 'unbreakable' or 'invincible'. Famous diamonds include the Hope Diamond, Cullinan Diamond, and Koh-i-Noor.
Field identification & locations
Identifying diamonds in the field can be challenging due to their often rough, unpolished appearance. Look for: Exceptional hardness: A diamond will scratch almost any other material. Density: It feels heavier than other minerals of similar size (specific gravity ~3.5). Luster: Even in rough form, a diamond often exhibits a greasy or waxy surface luster. Crystal shape: Uncut diamonds frequently show octahedral, dodecahedral, or cubic forms. Common locations: Major diamond-producing countries include Russia, Botswana, Canada, Australia, South Africa, and Angola. Diamonds are found in kimberlite pipes (primary deposits) and alluvial deposits (secondary deposits in rivers and ancient riverbeds). For collectors, rough diamonds offer unique natural beauty, while cut diamonds are prized for their sparkle and clarity. Always be wary of imitations when searching for or purchasing diamonds.
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