
metamorphic
Polished tiger’s eye
Quartz variety, SiO₂, with parallel fibrous amphibole pseudomorphs (crocidolite)
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; golden-brown to reddish-brown silky bands, vitreous-to-waxy luster, cryptocrystalline quartz, and chatoyant “cat’s-eye” sheen. No obvious cleavage; specific gravity about 2.6–2.7.
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Physical properties
Hardness 6.5–7 Mohs; golden-brown to reddish-brown silky bands, vitreous-to-waxy luster, cryptocrystalline quartz, and chatoyant “cat’s-eye” sheen. No obvious cleavage; specific gravity about 2.6–2.7.
Formation & geological history
Forms when quartz replaces fibrous blue asbestos (crocidolite) during low-grade alteration, preserving its parallel structure; commonly Precambrian in age. The specimen is tumbled and polished.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and inexpensive jewelry; not generally used as a construction stone.
Geological facts
Its moving band of reflected light is called chatoyancy and is strongest when cut or polished parallel to the fibers. Brown-gold tiger’s eye is commonly associated with blue hawk’s-eye and red tiger’s eye.
Field identification & locations
Identify by its undulating golden-brown bands and directional cat’s-eye flash, especially under a focused light. Major sources include South Africa, Western Australia, India, Namibia, and Thailand.
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