Corundum Mining


Corundum is a crystalline form of aluminum oxide (Al2O3) with traces of iron, titanium and chromium. It is a rock-forming mineral. It is one of the naturally transparent materials, but can have different colors when impurities are present. Transparent specimens are used as gems such as sapphires and rubies. Rubies are red due to traces of chromium in the corundum. All other colors of transparent corundum are called sapphires. Deep blue sapphires are blue due to the presence of titanium and iron.

Synthetic corundum was first created in 1837 and in 1903 the manufacture of corundum became more large scale. Originally synthesized to make rubies, now corundum is synthesized to make lenses for satellites, scratch resistant glass, and other high strength optical materials.

Geology: Corundum is a metamorphic variant of bauxite and therefore appears most commonly as a metamorphosed bauxite deposit, or as altered aluminous shale. It is unusually dense and nearly as hard as diamond. Gem quality corundum is found in streams as its high density causes pieces to deposit within one local region and its hardness makes it resistant to weathering.


Type Crystal System
Mineral Trigonal
Mineral Classification Color
Hematite Variable; colorless, yellow, orange, red, blue, violet, golden-brown, gray and green.
Chemical Formula Luster
Al2O3 Adamantine, vitreous, and/or pearly
Streak Fracture
White Conchoidal
Mohs Hardness

See aluminum.

Corundum is used as an abrasive because it has a hardness of 9.0 and can scratch almost anything. It is used in sandpaper and in industrial abrasives. However, in the U.S., synthetics have recently begun replacing natural corundum as the abrasive of choice. Its widest use in the US is for hardening heavy-duty concrete floors and for nonskid material on bridges. Because synthetic corundum is so hard and also transparent, it has many applications in optics and space equipment.

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