
mineral
Blue Topaz (specifically London Blue shade)
Topaz - Al2SiO4(F,OH)2
AI-generated identification · may be incorrectHardness: 8 on the Mohs scale; Color: Deep teal-blue; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Perfect basal; Specific Gravity: 3.4–3.6.
- Hardness
- 8 on the Mohs scale
- Color
- Deep teal-blue
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 8 on the Mohs scale; Color: Deep teal-blue; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Perfect basal; Specific Gravity: 3.4–3.6.
Formation & geological history
Formed in acidic igneous rocks like granite and rhyolite, often in pegmatite veins or cavaties. While natural blue topaz exists, most 'London Blue' specimens start as colorless topaz that is irradiated and heat-treated to achieve the deep color.
Uses & applications
Primarily used in jewelry (rings, pendants, earrings) due to its high hardness and clarity. It is also a popular collector's gemstone and the birthstone for December.
Geological facts
London Blue is the deepest and most valuable of the three standard treated blue topaz shades. Despite being common in the market, it takes roughly two years of cooling/aging after irradiation before the stone is safe for humans to wear.
Field identification & locations
In the field, it is identified by its high hardness, inability to be scratched by quartz, and heavy feel for its size (high specific gravity). It is commonly sourced from Brazil, Sri Lanka, and Nigeria.
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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