
mineral
Blue Zircon
Zirconium Silicate (ZrSiO4)
AI-generated identification · may be incorrectHardness: 7.5 (Mohs scale), Color: Vivid blue to cyan, Luster: Adamantine (diamond-like), Crystal structure: Tetragonal, Cleavage: Indistinct, Specific gravity: 4.6–4.7
- Hardness
- 7
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Physical properties
Hardness: 7.5 (Mohs scale), Color: Vivid blue to cyan, Luster: Adamantine (diamond-like), Crystal structure: Tetragonal, Cleavage: Indistinct, Specific gravity: 4.6–4.7
Formation & geological history
Zircon forms as a primary mineral in igneous rocks like granite and pegmatite. Blue zircon is specifically produced through the heat treatment of naturally occurring brown zircon specimens, often found in alluvial deposits dating back millions of years.
Uses & applications
Primarily used as a gemstone in high-end jewelry (rings, pendants) due to its exceptional fire and brilliance. Also used as an industrial source of zirconium and a geochronological tool for dating the Earth's crust.
Geological facts
Zircon is the oldest mineral on Earth, with some specimens dated to 4.4 billion years old. Blue zircon was a favorite during the Victorian era and is the birthstone for December.
Field identification & locations
Identify by its high refractive index and noticeable double refraction (facet edges will appear doubled when viewed through the stone). Commonly found in Cambodia, Sri Lanka, and Myanmar. Use a loupe to check for 'doubling' and internal inclusions.
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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