mineral

Blue Topaz

Al2SiO4(F,OH)2 (Fluorine-bearing aluminum silicate)

Hardness: 8 on Mohs scale; Color: Light blue to deep 'Swiss' or 'London' blue; Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Perfect basal cleavage; Specific Gravity: 3.4–3.6.

Hardness: 8 on Mohs scale
Color: Light blue to deep 'Swiss' or 'London' blue
Luster: Vitreous (glassy)

Identified April 15, 2026More mineral →

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Physical properties

Formation & geological history

Formed in granitic pegmatites and rhyolites via fluorine-bearing vapors during late-stage igneous crystallization; often found in alluvial deposits. Age varies by formation location (e.g., millions of years in Brazil).

Uses & applications

Primarily used in high-end jewelry as a gemstone. Also used as a specimen for mineral collectors. Industrially, it has limited use due to cleavage but is occasionally used in abrasive applications.

Geological facts

Natural blue topaz is actually quite rare; most of the vibrant blue topaz on the market today is created by treating colorless or pale yellow topaz with irradiation followed by heating. It is the birthstone for December.

Field identification & locations

Identify by its hardness (scratches glass/quartz easily), high refractive index, and perfectly flat cleavage surfaces. Often found in Brazil, Nigeria, and Sri Lanka. Collectors look for clarity and intensity of color.

Other mineral specimens

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Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Schist

Metamorphic

Epidote

Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)

metamorphic

Nephrite Jade

Nephrite

Mineral/Rock

Banded Gneiss (River Rock/Pebble)

Gneiss (specifically a banded variety often found as a river rock)

Metamorphic Rock

Green Apatite on Albite

Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]

mineral