
metamorphic
Tumbled tiger’s-eye
Quartz variety with fibrous crocidolite pseudomorphs; SiO₂
AI-generated identification · may be incorrectMohs hardness 6.5–7; golden-brown chatoyant bands, vitreous to silky luster, translucent edges, and no obvious cleavage. Its polished surface produces a moving cat’s-eye sheen when rotated in light.
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Physical properties
Mohs hardness 6.5–7; golden-brown chatoyant bands, vitreous to silky luster, translucent edges, and no obvious cleavage. Its polished surface produces a moving cat’s-eye sheen when rotated in light.
Formation & geological history
Forms when blue asbestos-like crocidolite fibers are replaced by quartz during low-grade metamorphism, commonly in Precambrian rocks; major deposits occur in South Africa, Western Australia, India, and Namibia.
Uses & applications
Used for cabochons, beads, carvings, decorative objects, and inexpensive tumbled stones; it is generally valued as an ornamental gemstone rather than for industrial use.
Geological facts
The chatoyancy results from aligned fibrous inclusions reflecting light. Golden tiger’s-eye commonly develops through alteration of blue hawk’s-eye material, with iron oxides producing the yellow-brown color.
Field identification & locations
Identify it by its parallel silky bands and strong sliding cat’s-eye effect, distinguishing it from ordinary quartz or jasper. The image shows a polished/tumbled piece, likely tiger’s-eye, though exact identification would benefit from examining the chatoyancy under a direct light.
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