
mineral
White Sapphire
Corundum (Al2O3)
AI-generated identification · may be incorrectHardness: 9 on Mohs scale; Color: Colorless/Transparent; Luster: Adamantine to vitreous; Crystal system: Trigonal; Cleavage: None (has parting); Specific Gravity: 3.95-4.10
- Hardness
- 9 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Colorless/Transparent; Luster: Adamantine to vitreous; Crystal system: Trigonal; Cleavage: None (has parting); Specific Gravity: 3.95-4.10
Formation & geological history
Formed in aluminum-rich metamorphic rocks (schist, gneiss) and igneous rocks (syenites, pegmatites) under high pressure and temperature. Primary sources are alluvial deposits (river beds) or pipe deposits.
Uses & applications
Used primarily in fine jewelry as a diamond alternative, industrial abrasives, watch crystals, and high-durability optical windows.
Geological facts
Sapphire is the same mineral as Ruby; the only difference is the trace element that provides color. White sapphire is the purest form of corundum, lacking the chemical impurities that create blue or red hues.
Field identification & locations
Identify in the field by its extreme hardness (will scratch glass and topaz easily) and heavy weight for its size. Major locations include Sri Lanka, Madagascar, and Myanmar. Professional gemological testing is needed to distinguish it from White Zircon or Synthetic Moissanite.
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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