
mineral
Corundum (Sapphire variant)
Aluminium oxide (Al2O3)
Hardness: 9 on Mohs scale; Color: Grayish-brown to dull greenish-blue; Luster: Adamantive to vitreous (can appear greasy when worn); Crystal structure: Trigonal/Hexagonal; Cleavage: None (has parting); Specific gravity: 3.95–4.10.
- Hardness
- 9 on Mohs scale
- Color
- Grayish-brown to dull greenish-blue
- Luster
- Adamantive to vitreous (can appear greasy when worn)
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Physical properties
Hardness: 9 on Mohs scale; Color: Grayish-brown to dull greenish-blue; Luster: Adamantive to vitreous (can appear greasy when worn); Crystal structure: Trigonal/Hexagonal; Cleavage: None (has parting); Specific gravity: 3.95–4.10.
Formation & geological history
Formed as a primary mineral in igneous rocks like syenite and pegmatite, or in metamorphic rocks such as mica schist and gneiss. Often found in alluvial deposits (placer deposits) due to its extreme hardness and resistance to weathering.
Uses & applications
Non-gem quality corundum is used heavily as an industrial abrasive. Low-grade specimens are popular for gemstone tumbling practice or as reference mineral specimens for collectors.
Geological facts
Corundum is the second hardest natural mineral known to man, behind only diamond. While red corundum is called ruby, all other colors are technically sapphires. Stones with this specific barrel-like shape are often referred to as 'corundum crystals' or 'sapphire rough'.
Field identification & locations
Identify in the field by its characteristic barrel shape (hexagonal bipyramidal), extreme heaviness for its size, and the fact that it will easily scratch glass, quartz, and topaz. Commonly found in riverbeds in Montana, North Carolina, and Southeast Asia.
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