Rock Identifier
White Topaz (Aluminum silicate fluoride hydroxide (Al2SiO4(F,OH)2)) — mineral
mineral

White Topaz

Aluminum silicate fluoride hydroxide (Al2SiO4(F,OH)2)

Hardness: 8 on the Mohs scale; Color: Colorless (white); Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Perfect basal cleavage; Specific Gravity: 3.4 to 3.6.

Hardness
8 on the Mohs scale
Color
Colorless (white)
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 8 on the Mohs scale; Color: Colorless (white); Luster: Vitreous (glassy); Crystal Structure: Orthorhombic; Cleavage: Perfect basal cleavage; Specific Gravity: 3.4 to 3.6.

Formation & geological history

Formed as a result of fluorine-rich vapors given off during the final stages of the crystallization of igneous rocks (primarily granites and pegmatites). It can also be found in alluvial deposits. Geological age varies by location, occurring in Precambrian to Cenozoic formations.

Uses & applications

Major use in the jewelry industry as a diamond substitute due to its hardness and clarity. Also used as a gemstone for collectors and industrial applications requiring high-temperature stability.

Geological facts

Topaz is the state gemstone of Utah and the birthstone for November. In ancient times, the Greeks believed it gave them strength, and in the Middle Ages, Europeans thought it could dispel spells and anger.

Field identification & locations

Identify in the field by its high hardness (it cuts glass easily), its orthorhombic crystal habit (typically prismatic), and its weight (higher specific gravity than quartz). Common locations include Brazil, Russia, Sri Lanka, and the United States (Texas and Colorado).