
metamorphic
Polished golden-brown banded stone, likely tiger’s eye
Tiger’s eye (quartz with fibrous crocidolite pseudomorphs; SiO₂)
AI-generated identification · may be incorrectGolden to ochre bands with dark seams and a silky chatoyant sheen; quartz hardness 7 Mohs, trigonal crystal structure, no prominent cleavage, specific gravity about 2.6. The image appears to show a cut or polished slab, though the exact stone is uncertain from appearance alone.
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Physical properties
Golden to ochre bands with dark seams and a silky chatoyant sheen; quartz hardness 7 Mohs, trigonal crystal structure, no prominent cleavage, specific gravity about 2.6. The image appears to show a cut or polished slab, though the exact stone is uncertain from appearance alone.
Formation & geological history
Forms when silica replaces fibrous crocidolite during low-grade alteration, preserving its banded structure; many commercial specimens come from South Africa and western Australia. The age depends on the host deposit.
Uses & applications
Used for cabochons, beads, decorative slabs, and carvings; polished material is valued for its shifting reflective bands.
Geological facts
Tiger’s eye’s moving, cat-like band of light is called chatoyancy and results from aligned fibers.
Field identification & locations
Look for parallel golden-brown bands and a silky light stripe that shifts when the stone is tilted; a smooth, flat slab cut does not show enough detail for confident identification. Common sources include South Africa, Australia, India, and Namibia.
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