Rock Identifier
Blue Sapphire (Corundum (Al2O3) with traces of Iron and Titanium) — mineral
mineral

Blue Sapphire

Corundum (Al2O3) with traces of Iron and Titanium

Hardness: 9 on the Mohs scale. Color: Deep royal blue (exhibiting pleochroism). Luster: Vitreous to Adamantine. Crystal Structure: Hexagonal (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 3.98 - 4.06.

Hardness
9 on the Mohs scale
Color
Deep royal blue (exhibiting pleochroism)
Luster
Vitreous to Adamantine
Identified More mineral

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Physical properties

Hardness: 9 on the Mohs scale. Color: Deep royal blue (exhibiting pleochroism). Luster: Vitreous to Adamantine. Crystal Structure: Hexagonal (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 3.98 - 4.06.

Formation & geological history

Formed in metamorphic rocks (schist, gneiss) or igneous rocks (alkali basalt, syenite) under high pressure and temperature. Commonly found in secondary alluvial deposits (gem gravels). Geological ages vary widely from Pan-African (approx. 500-600 Ma) to Cenozoic.

Uses & applications

Primarily used as a gemstone in high-end jewelry (rings, necklaces). Industrial grade sapphires are used for scratch-resistant watch crystals, optical components, and abrasives.

Geological facts

Sapphire is the birthstone for September. The blue color is the result of intervalence charge transfer between Fe2+ and Ti4+ ions. Famous specimens include the 'Star of India' and the 'Logan Sapphire'.

Field identification & locations

Identify in the field by high density, extreme hardness (scratches almost all other minerals), and typical hexagonal barrel-shaped crystal habit. Common locations include Sri Lanka, Madagascar, Myanmar (Burma), and Montana, USA.