
Mineral
Diamond
Diamond (a metastable allotrope of carbon, C)
Hardness: 10 (Mohs scale), the hardest known natural mineral. Color: Typically colorless or yellow, but can be blue, green, brown, pink, red, orange, or black. Luster: Adamantine (brilliant, like a highly polished diamond). Crystal Structure: Isometric (cubic) system, often forms octahedral or dodecahedral crystals.…
- Hardness
- 10 (Mohs scale), the hardest known natural mineral
- Luster
- Adamantine (brilliant, like a highly polished diamond)
Identified More mineral →
Explore Diamond in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 10 (Mohs scale), the hardest known natural mineral. Color: Typically colorless or yellow, but can be blue, green, brown, pink, red, orange, or black. Luster: Adamantine (brilliant, like a highly polished diamond). Crystal Structure: Isometric (cubic) system, often forms octahedral or dodecahedral crystals. Cleavage: Perfect octahedral cleavage (though not easily induced due to hardness and strong covalent bonds). Specific Gravity: 3.51.
Formation & geological history
Diamonds form under extremely high pressure and temperature conditions deep within the Earth's mantle, typically at depths of 150-200 km (90-120 miles). They are brought to the surface through deep-seated volcanic eruptions, often in kimberlite or lamproite pipes. Most natural diamonds are billions of years old, predating the formation of life on Earth.
Uses & applications
Industry: Abrasives, cutting tools, drilling bits, polishing agents, wire drawing dies. Jewelry: Highly valued as gemstones for rings, necklaces, earrings, and other ornaments. Science/Technology: Diamond anvils for high-pressure experiments, heat sinks for electronic devices due to high thermal conductivity, optical windows.
Geological facts
Diamonds are the hardest natural substance on Earth, making them ideal for industrial cutting and grinding. They are also highly prized as gemstones due to their exceptional brilliance and fire. The largest gem-quality diamond ever found is the Cullinan Diamond, weighing 3,106.75 carats (621.35 grams) in its rough state.
Field identification & locations
Diamonds are identified in the field by their extreme hardness (they can scratch any other mineral), adamantine luster, and often characteristic octahedral crystal habit. They are primarily found in ancient cratonic regions of the world, specifically in kimberlite and lamproite pipes, as well as in alluvial deposits where they have been weathered out of their primary source rocks. Major diamond-producing countries include Russia, Botswana, Canada, Australia, and South Africa. For collectors, rough diamond crystals are sought after, while cut and polished diamonds are valued based on the 'four C's': Carat weight, Cut, Color, and Clarity.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous