
mineral
Tiger's Eye
Pseudomorph of Quartz after Crocidolite (SiO2)
Hardness: 7 (Mohs); Color: Golden-brown to yellow-gold; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Notable for its chatoyancy or 'cat's eye' effect.
- Hardness
- 7 (Mohs)
- Color
- Golden-brown to yellow-gold
- Luster
- Silky
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Physical properties
Hardness: 7 (Mohs); Color: Golden-brown to yellow-gold; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Notable for its chatoyancy or 'cat's eye' effect.
Formation & geological history
Formed through a pseudomorphic process where silica (Quartz) replaces the fibrous mineral Crocidolite while retaining the original fibrous structure. Most deposits are found in Precambrian iron formations around 2 billion years old.
Uses & applications
Primarily used in jewelry (cabochons, beads), decorative carvings, lapidary arts, and as a popular specimen for crystal collectors.
Geological facts
It is a chatoyant gemstone that exhibits a unique silky luster due to the parallel growth of quartz crystals and altered amphibole fibers. 'Blue Tiger\'s Eye' is known as Hawk\'s Eye and represents a stage where the asbestos fibers have not yet been oxidized by iron.
Field identification & locations
Identify by its distinctive bands of gold and brown and its optical chatoyancy when rotated under light. Major locations include South Africa (Northern Cape), Australia, Myanmar, and Namibia.
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