Rock Identifier
Polished tiger’s-eye and jasper specimen (Quartz (SiO₂), chiefly fibrous chatoyant quartz, with iron-oxide-rich jasper/goethite) — gemstone
gemstone

Polished tiger’s-eye and jasper specimen

Quartz (SiO₂), chiefly fibrous chatoyant quartz, with iron-oxide-rich jasper/goethite

AI-generated identification · may be incorrect

Hardness about 6.5–7 (quartz); golden-brown bands show silky chatoyancy, while the darker brown material is opaque and earthy to subvitreous. The specimen appears polished or tumbled, obscuring natural crystal faces and cleavage.

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Physical properties

Hardness about 6.5–7 (quartz); golden-brown bands show silky chatoyancy, while the darker brown material is opaque and earthy to subvitreous. The specimen appears polished or tumbled, obscuring natural crystal faces and cleavage.

Formation & geological history

Tiger’s-eye forms when crocidolite fibers are replaced by quartz and iron oxides during low-grade alteration, commonly in Precambrian metamorphic rocks; associated jasper forms from silica- and iron-rich sedimentary or hydrothermal material. Major deposits occur in South Africa, Australia, India, and Namibia.

Uses & applications

Used for cabochons, beads, carvings, ornamental objects, and collector specimens; jasper is also used decoratively and occasionally as aggregate.

Geological facts

The golden sheen results from reflection along aligned microscopic fibers, producing chatoyancy similar to a cat’s eye. Blue hawk’s-eye is the less-oxidized precursor to golden tiger’s-eye.

Field identification & locations

Identify by its parallel silky bands, golden-to-brown color, opaque body, and glassy hardness; a polished surface and fibrous chatoyant sheen distinguish it from ordinary brown jasper. The image is too limited for precise species identification.