
mineral
White Zircon
Zircon (Zirconium silicate, ZrSiO4)
AI-generated identification · may be incorrectHardness: 7.5 on Mohs scale; Color: Colorless (White); Luster: Adamantine (diamond-like); Crystal Structure: Tetragonal; Cleavage: Indistinct; Specific Gravity: 4.6–4.7; High dispersion (fire).
- Hardness
- 7
- Color
- Colorless (White)
- Luster
- Adamantine (diamond-like)
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Physical properties
Hardness: 7.5 on Mohs scale; Color: Colorless (White); Luster: Adamantine (diamond-like); Crystal Structure: Tetragonal; Cleavage: Indistinct; Specific Gravity: 4.6–4.7; High dispersion (fire).
Formation & geological history
Formed in igneous rocks (granites, pegmatites) and metamorphic rocks. As it is very durable, it is often found in sedimentary deposits like 'gem gravels'. Some specimens are billions of years old.
Uses & applications
Primary source of zirconium metal; high-quality faceted stones are used in jewelry as a diamond alternative; used in industrial refractory applications and casting molds.
Geological facts
Zircon is the oldest known mineral on Earth, with some grains dated to 4.4 billion years. It contains trace amounts of uranium and thorium, which geologists use for radiometric dating.
Field identification & locations
Identify in the field by its high luster, specific gravity, and 'doubling' of facet edges when viewed through the table due to high birefringence. Found in Sri Lanka, Cambodia, Myanmar, and Australia.
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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