
mineral
Imperial Topaz
Al2SiO4(F,OH)2
AI-generated identification · may be incorrectHardness: 8.0 (Mohs scale); Color: Golden yellow to orange-peach; Luster: Vitreous; Crystal system: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.4 - 3.6
- Hardness
- 8
- Color
- Golden yellow to orange-peach
- Luster
- Vitreous
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Physical properties
Hardness: 8.0 (Mohs scale); Color: Golden yellow to orange-peach; Luster: Vitreous; Crystal system: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.4 - 3.6
Formation & geological history
Formed as a silicate mineral in igneous rocks such as pegmatite and rhyolite, or in cavities in sedimentary rocks. High-quality imperial topaz is most famously associated with the Ouro Preto region of Brazil.
Uses & applications
Primarily used as a gemstone in high-end jewelry and as a sought-after specimen for mineral collectors.
Geological facts
Imperial Topaz is the rarest and most valuable variety of topaz. Its name comes from the Russian Tsars of the 19th century who claimed exclusive rights to the pink topaz mined in Russia.
Field identification & locations
Identify by its high hardness (it will scratch quartz), distinct orange-golden hue, and vertical striations on the crystal faces. Common locations include Brazil, Pakistan, and Russia.
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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