![Rough Topaz (Aluminum silicate fluoride hydroxide [Al2SiO4(F, OH)2]) — mineral](https://media.rockidentification.com/e8521fcb-569c-414d-9b83-1387f0b4bc90-compressed.jpg)
mineral
Rough Topaz
Aluminum silicate fluoride hydroxide [Al2SiO4(F, OH)2]
Hardness: 8.0 on Mohs scale; Color: Yellow, honey-brown, or colorless (as shown); Luster: Vitreous; Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.4 to 3.6
- Hardness
- 8
- Color
- Yellow, honey-brown, or colorless (as shown)
- Luster
- Vitreous
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Physical properties
Hardness: 8.0 on Mohs scale; Color: Yellow, honey-brown, or colorless (as shown); Luster: Vitreous; Crystal structure: Orthorhombic; Cleavage: Perfect basal; Specific gravity: 3.4 to 3.6
Formation & geological history
Formed through fluorine-bearing vapors given off during the last stages of the crystallization of igneous rocks. It is most commonly found in cavities of granitic pegmatites, rhyolites, and secondary alluvial deposits.
Uses & applications
Primary use is in jewelry as a gemstone. It is also a minor industrial source of fluorine and is highly sought after by mineral collectors for its crystal clarity and diverse colors.
Geological facts
Topaz is one of the hardest of all naturally occurring minerals. Historically, all yellow gems were called topaz; however, true topaz is chemically distinct and much harder than citrine (quartz) which is often sold as 'topaz'.
Field identification & locations
Field identification is based on its high hardness (it will scratch quartz), distinct heavy feel (high specific gravity), and its tendency to break along a perfectly flat plane (basal cleavage). Found in regions like Brazil, Nigeria, Sri Lanka, and Utah (USA).
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