
mineral
Blue Sapphire Crystal (Rough)
Corundum (Aluminum Oxide, Al2O3)
AI-generated identification · may be incorrectHardness: 9 on Mohs scale; Color: Grayish-blue to deep blue with a tan/brown host rock or weathered crust; Luster: Adamantine to vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: No true cleavage but show prominent parting.
- Hardness
- 9 on Mohs scale
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Grayish-blue to deep blue with a tan/brown host rock or weathered crust; Luster: Adamantine to vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: No true cleavage but show prominent parting.
Formation & geological history
Formed under high-pressure, high-temperature conditions in regional metamorphism or from igneous melts (pegmatites). Often found in alluvial deposits or as primary crystals within schist, gneiss, or marble.
Uses & applications
When gem-quality, it is used for high-end jewelry. Industrial-grade corundum is used for abrasives, watch crystals, and specialized optical windows due to its extreme hardness.
Geological facts
Sapphire is the second hardest natural mineral after diamond. The color comes from trace elements of iron and titanium. Rough hexagonal prisms like this one often show 'silk' (rutile inclusions).
Field identification & locations
Identify by its 6-sided hexagonal barrel shape, extreme hardness (will scratch almost anything but diamond), and high density. Commonly found in Madagascar, Sri Lanka, and Montana, USA.
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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