
metamorphic
Polished tiger’s-eye
Quartz variety: fibrous chatoyant quartz, chiefly SiO₂, pseudomorphous after crocidolite
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; dark brown to golden-brown with silky chatoyancy, vitreous-to-waxy luster, and no obvious cleavage. The specimen appears polished and may include iron-oxide-rich bands or brecciation.
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Physical properties
Hardness about 6.5–7 Mohs; dark brown to golden-brown with silky chatoyancy, vitreous-to-waxy luster, and no obvious cleavage. The specimen appears polished and may include iron-oxide-rich bands or brecciation.
Formation & geological history
Forms when blue asbestos (crocidolite) fibers are replaced by quartz and oxidized to limonite/hematite, commonly during low-grade metamorphism. Major deposits occur in Precambrian rocks of South Africa and Western Australia.
Uses & applications
Used for cabochons, carvings, beads, ornamental stones, and inexpensive collector specimens; it is not generally used as a construction stone.
Geological facts
Its moving cat’s-eye stripe results from aligned fibrous inclusions reflecting light. Golden tiger’s-eye is commonly intergrown with blue hawk’s-eye and red-brown iron-rich zones.
Field identification & locations
Identify it by its polished silky bands and strong light-reflecting chatoyancy, unlike ordinary brown jasper. Common sources include South Africa, Western Australia, India, and Thailand.
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