
mineral
Diamond
Carbon (C)
Hardness: 10 (Mohs scale), Color: Colorless (as shown) but can be various hues, Luster: Adamantine, Crystal Structure: Isometric-Hexoctahedral, Cleavage: Octahedral (perfect in 4 directions), Specific Gravity: 3.51
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 10 (Mohs scale), Color: Colorless (as shown) but can be various hues, Luster: Adamantine, Crystal Structure: Isometric-Hexoctahedral, Cleavage: Octahedral (perfect in 4 directions), Specific Gravity: 3.51
Formation & geological history
Formed under extreme high pressure and temperature conditions deep in Earth's mantle, approximately 100 miles below the surface. They are brought to the surface via volcanic eruptions in kimberlite and lamproite pipes.
Uses & applications
Predominantly used in jewelry as gemstones. Industrial uses include cutting, drilling, grinding, and polishing tools due to its extreme hardness as an abrasive.
Geological facts
Diamonds are the hardest known natural material. Most natural diamonds are between 1 billion and 3.5 billion years old. The name comes from the Greek word 'adamas', meaning invincible.
Field identification & locations
Identify in the field by its extreme hardness (cannot be scratched by any other material) and its specific luster. Commonly found in secondary alluvial deposits or primary kimberlite pipes. Use a thermal conductivity probe (diamond tester) for verification.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral