
mineral
Blue Topaz
Aluminum silicate fluoride hydroxide (Al2SiO4(F,OH)2)
AI-generated identification · may be incorrectHardness: 8.0 on the Mohs scale; Color: Sky blue to electric blue; Luster: Vitreous (glass-like); Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.49–3.57.
- Hardness
- 8
- Color
- Sky blue to electric blue
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 8.0 on the Mohs scale; Color: Sky blue to electric blue; Luster: Vitreous (glass-like); Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.49–3.57.
Formation & geological history
Formed in igneous rocks like pegmatites and rhyolites during the late stages of magmatic crystallization, often from fluorine-bearing vapors. Commonly found in alluvial deposits. Geological age varies significantly by deposit.
Uses & applications
Primarily used in jewelry for pendants, rings, and earrings. Also used as a birthstone and by collectors as faceted specimens.
Geological facts
Natural blue topaz is rare; most blue topaz on the market is clear topaz that has been irradiated and heat-treated to achieve the blue color. The 'Swiss Blue' and 'London Blue' are famous trade names for these colors.
Field identification & locations
Identify by its high hardness (it can scratch glass and quartz) and its high density. It has a distinctive slippery feel. Found commonly in Brazil, USA (pikes peak), and Sri Lanka.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary