
mineral
Polished tiger’s-eye pebble
Quartz (SiO₂), chatoyant fibrous variety; commonly partly altered crocidolite
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; golden-brown to dark brown bands with silky, reflective chatoyancy; vitreous to silky luster, typically microcrystalline and without visible cleavage. Specific gravity is about 2.6–2.7.
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Physical properties
Hardness 6.5–7 Mohs; golden-brown to dark brown bands with silky, reflective chatoyancy; vitreous to silky luster, typically microcrystalline and without visible cleavage. Specific gravity is about 2.6–2.7.
Formation & geological history
Forms when fibrous blue asbestos (crocidolite) is replaced by quartz during hydrothermal alteration, preserving the fibers and producing the cat’s-eye effect. Most gem material formed in Precambrian rocks, especially South Africa and Western Australia.
Uses & applications
Commonly tumbled, carved, and used in cabochon jewelry, beads, ornaments, and metaphysical collections; usually inexpensive.
Geological facts
The bright band moves across the surface when the stone is rotated relative to light, caused by aligned fibers. This small specimen appears polished or tumbled rather than naturally weathered.
Field identification & locations
Identify it by its golden chatoyant stripe, brown-gold color, quartz-like hardness, and lack of cleavage; distinguish it from brown glass by its natural fibrous banding and cooler feel. Major sources include South Africa, Australia, India, and Thailand.
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