Rock Identifier
Diamond (Diamond (C)) — Mineral
Mineral

Diamond

Diamond (C)

Hardness: 10 (Mohs scale), the hardest known natural material. Color: Pure diamonds are colorless, but impurities can lead to yellow, brown, green, blue, pink, red, and black. Luster: Adamantine (brilliant, diamond-like). Crystal structure: Isometric (typically octahedral, dodecahedral, or cubic).…

Hardness
10 (Mohs scale), the hardest known natural material
Luster
Adamantine (brilliant, diamond-like)
Identified More mineral

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Physical properties

Hardness: 10 (Mohs scale), the hardest known natural material. Color: Pure diamonds are colorless, but impurities can lead to yellow, brown, green, blue, pink, red, and black. Luster: Adamantine (brilliant, diamond-like). Crystal structure: Isometric (typically octahedral, dodecahedral, or cubic). Cleavage: Perfect octahedral cleavage (though rarely observed due to extreme hardness). Specific gravity: 3.5-3.53.

Formation & geological history

Diamond formation occurs in the Earth's mantle at depths of 150-200 km (93-124 miles), under extremely high pressures (45-60 kilobars) and temperatures (900-1300 °C). These conditions allow carbon atoms to bond in a strong, rigid crystal lattice. Diamonds are brought to the Earth's surface through explosive volcanic eruptions, often in kimberlite and lamproite pipes, which are carrot-shaped igneous intrusions. The geological age of diamonds can range from hundreds of millions to over 3 billion years, making them among the oldest minerals on Earth.

Uses & applications

Industry: Cutting, grinding, and drilling tools; optical windows; heat sinks; abrasive powders. Jewelry: Highly prized as gemstones for rings, necklaces, earrings, and other ornaments due to their unparalleled brilliance and hardness. Construction: Used in diamond-tipped tools for cutting concrete and asphalt.

Geological facts

Diamonds are the hardest natural substance. They form deep within the Earth's mantle and are brought to the surface through volcanic eruptions. Each diamond contains billions of carbon atoms arranged in an extremely stable crystal lattice. They are valued for their brilliance, fire, and scintillation.

Field identification & locations

Diamonds are identified by their extreme hardness (they scratch all other minerals), adamantine luster, and typical crystal habits (octahedral, dodecahedral). They often exhibit high dispersion (fire). Common locations include South Africa, Botswana, Russia, Canada, Australia, and Brazil, primarily found in kimberlite pipes or alluvial deposits. For collectors, raw diamond crystals are sought after, while cut and polished diamonds are valued based on the '4Cs': Carat (weight), Cut (proportions and finish), Color (absence of color), and Clarity (absence of inclusions).