Blue Topaz
Al2SiO4(F,OH)2 (Fluorine-bearing aluminum silicate)
Rock Type: mineral

Physical Properties
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.
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.
Identified on: 4/15/2026
Mode: Standard