
mineral
Titanium Quartz (Rough)
Titanium-included Silicon Dioxide (SiO2 + Ti)
Hardness: 7 (Mohs scale); Color: Brownish-tan to smoky grey with potential internal metallic rutilations; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Brownish-tan to smoky grey with potential internal metallic rutilations; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in igneous or metamorphic environments through hydrothermal processes where titanium-rich fluids (often rutile) are trapped within cooling silica. The specimen appears to be raw ('brut') or water-worn.
Uses & applications
Predominantly used for lapidary work, jewelry making (cabochons), and as a collector's specimen. In industry, pure quartz is used for electronics and glassmaking, though this specific variety is ornamental.
Geological facts
The label 'quartz titane brut' is French for raw titanium quartz. When titanium occurs as needle-like inclusions within quartz, it is known as rutilated quartz. If the titanium is bonded to the surface via a vacuum process, it is called 'Aura Quartz,' though this specimen appears natural.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and characteristic inclusions. Commonly found in Brazil, Madagascar, and the Swiss Alps. Collectors should look for internal 'needles' or smoky coloration indicating mineral impurities.
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