
mineral
Topaz
Al2SiO4(F,OH)2
Hardness: 8 (Mohs), Color: Colorless, pale blue, yellow, yellowish brown, orange, pinkish red; Luster: Vitreous; Crystal structure: Orthorhombic; Cleavage: Perfect on {001}; Specific gravity: 3.49 - 3.57.
- Luster
- Vitreous
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Physical properties
Hardness: 8 (Mohs), Color: Colorless, pale blue, yellow, yellowish brown, orange, pinkish red; Luster: Vitreous; Crystal structure: Orthorhombic; Cleavage: Perfect on {001}; Specific gravity: 3.49 - 3.57.
Formation & geological history
Commonly occurs in fluorine-bearing, highly silicic igneous rocks like granite, granite pegmatite, and rhyolite. It also forms in cavities of volcanic rocks, hydrothermal veins, and greisens.
Uses & applications
Predominantly used as a gemstone. Lesser quality or massive forms are uncommonly used as a source for aluminum.
Geological facts
Topaz is the state gem of Utah and the birthstone for November (yellow) or December (blue). Imperial topaz is highly prized.
Field identification & locations
Field identification often relies on its characteristic orthorhombic crystalline form, its high hardness of 8 (scratching quartz), perfect basal cleavage, and high specific gravity. Commonly found worldwide, major localities include Brazil, Russia, Sri Lanka, USA (Utah, Colorado), and Mexico. While found in Illinois, gem-grade crystals like this are rare and could be from elsewhere.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral