
mineral
Blue Sapphire
Corundum (Al2O3)
AI-generated identification · may be incorrectHardness: 9 on Mohs scale; Color: Deep blue (the 'primary' color for sapphires caused by iron and titanium); Luster: Adamantine to vitreous; Crystal Structure: Trigonal; Cleavage: None (has parting); Specific Gravity: 3.98–4.06.
- Hardness
- 9 on Mohs scale
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Deep blue (the 'primary' color for sapphires caused by iron and titanium); Luster: Adamantine to vitreous; Crystal Structure: Trigonal; Cleavage: None (has parting); Specific Gravity: 3.98–4.06.
Formation & geological history
Formed in aluminum-rich metamorphic rocks (schists/gneisses) or igneous rocks (syenites/pegmatites). Common in alluvial deposits where heavy minerals settle. Most geological deposits range from 500 million to a billion years old.
Uses & applications
Primarily used as a gemstone in high-end jewelry. Industrial varieties (synthetic sapphire) are used for scratch-resistant watch crystals, optical components, and abrasives.
Geological facts
Sapphire is the second hardest natural substance after diamond. The blue variety is the most famous, but sapphires come in every color except red (red corundum is classified as ruby).
Field identification & locations
Identify by its extreme hardness (cannot be scratched by steel or quartz) and high density. Commonly found in Sri Lanka, Madagascar, Myanmar, and Montana (USA). Collectors look for 'cornflower' or 'royal' blue shades with high clarity.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous