
metamorphic
Tumbled tiger’s-eye-rich metamorphic stone
Tiger’s eye: fibrous quartz (SiO₂), commonly intergrown with crocidolite pseudomorphs; possibly mixed with dark iron-rich matrix
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; brown-gold and black bands, vitreous to silky luster, opaque, compact microcrystalline structure, no obvious cleavage, specific gravity about 2.6–2.8. The polished surface may show subdued chatoyancy (cat’s-eye effect).
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Physical properties
Hardness about 6.5–7 Mohs; brown-gold and black bands, vitreous to silky luster, opaque, compact microcrystalline structure, no obvious cleavage, specific gravity about 2.6–2.8. The polished surface may show subdued chatoyancy (cat’s-eye effect).
Formation & geological history
Forms when blue asbestos-like crocidolite fibers are replaced by quartz and oxidized to golden-brown iron oxides during metamorphism. Major deposits are Proterozoic, especially in South Africa and Western Australia.
Uses & applications
Used as a lapidary and ornamental stone for cabochons, beads, carvings, and tumbled specimens; not generally used structurally.
Geological facts
Tiger’s eye is a pseudomorph: quartz preserves the fibrous texture of an earlier mineral. Strong chatoyancy is best seen under a single bright light moved across the surface.
Field identification & locations
Identify by parallel silky bands, brown-gold color, quartz-like hardness, and resistance to scratching by steel; this piece appears unusually dark and may be tiger’s eye mixed with matrix or another iron-rich stone. Common sources include South Africa, Australia, India, Brazil, and Namibia.
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