
metamorphic
Tiger's Eye
Pseudomorph of Quartz after Crocidolite (SiO2 with iron inclusions)
Hardness: 6.5-7 Mohs; Color: Golden yellow to brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Notable for chatoyancy.
- Hardness
- 6
- Color
- Golden yellow to brown
- Luster
- Silky
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Physical properties
Hardness: 6.5-7 Mohs; Color: Golden yellow to brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Notable for chatoyancy.
Formation & geological history
Formed through the pseudomorphism of crocidolite (asbestos) by silica. The original fibrous structure is preserved while being replaced by quartz, with iron oxidation producing the golden-brown hues. Most deposits are found in Precambrian rock units.
Uses & applications
Primarily used as a gemstone in jewelry (beads, cabochons), carvings, and ornamental objects. It is also a popular specimen for crystal healing collectors.
Geological facts
Tiger's Eye exhibits an optical effect known as chatoyancy or the 'cat\'s eye effect,' caused by the reflection of light off the parallel mineral fibers. If the stone is heated, it turns red (Red Tiger\'s Eye), and if naturally oxidized differently, it may remain blue (Hawk\'s Eye).
Field identification & locations
Identify by its characteristic moving bands of light (silkiness) and yellow/gold/brown color scheme. It is most commonly found in South Africa, Australia, India, and Burma. Collectors look for sharp, clean chatoyancy without dull spots.
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