
mineral
White Topaz
Topaz - Al2SiO4(F,OH)2
AI-generated identification · may be incorrectHardness: 8 on Mohs scale; Color: Colorless (White); Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific Gravity: 3.49–3.57.
- Hardness
- 8 on Mohs scale
- Color
- Colorless (White)
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 8 on Mohs scale; Color: Colorless (White); Luster: Vitreous (glassy); Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific Gravity: 3.49–3.57.
Formation & geological history
Formed in late-stage igneous processes within highly silicic rocks like granite and pegmatites, or in rhyolite cavities. Often found in vapor-rich environments where fluorine exists.
Uses & applications
Commonly used in the jewelry industry as a budget-friendly alternative to diamond. Also used occasionally in industrial optics and for mineral collecting.
Geological facts
Topaz is one of the hardest minerals in nature. While colorless in its pure form, natural imperfections and radiation can create a rainbow of colors; white topaz can be 'treated' with irradiation and heat to turn deep blue.
Field identification & locations
Identify by its high hardness (it will scratch quartz but not corundum) and its smooth, perfect basal cleavage. Common locations include Brazil, Russia, Pakistan, and the United States (Texas and Utah).
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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