
metamorphic
Tumbled tiger’s-eye
Quartz (SiO₂) with crocidolite-derived fibers and iron oxides
AI-generated identification · may be incorrectMohs hardness 6.5–7; golden-brown chatoyant bands, vitreous-to silky luster, opaque, microcrystalline quartz, no obvious cleavage; specific gravity about 2.6–2.7.
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Physical properties
Mohs hardness 6.5–7; golden-brown chatoyant bands, vitreous-to silky luster, opaque, microcrystalline quartz, no obvious cleavage; specific gravity about 2.6–2.7.
Formation & geological history
A fibrous quartz replacement formed when crocidolite asbestos fibers were silicified and later oxidized to iron-rich brown-gold colors, typically in Precambrian metamorphic rocks. Major deposits occur in South Africa, Western Australia, and Namibia.
Uses & applications
Commonly tumbled for collections and carved into cabochons, beads, and ornamental objects; relatively inexpensive jewelry stone.
Geological facts
Its shifting “cat’s-eye” sheen is called chatoyancy and is strongest when the stone is polished parallel to the aligned fibers.
Field identification & locations
Identify it by the silky, moving band of reflected light and golden-brown to reddish-brown coloration; unlike glass, it commonly shows fibrous bands and variable translucency. Typical specimens are a few dollars; quality cabochons or large polished pieces range from about $10–$75.
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