Rock Identifier
Tiger's Eye (Silicon Dioxide (Quartz pseudomorph after crocidolite), $SiO_2$) — mineral
mineral

Tiger's Eye

Silicon Dioxide (Quartz pseudomorph after crocidolite), $SiO_2$

Hardness of 7 on the Mohs scale, colors range from golden-brown to yellow-brown with characteristic chatoyancy (silky luster), trigonal crystal system, indistinct cleavage, and a specific gravity of around 2.64 to 2.71.

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Physical properties

Hardness of 7 on the Mohs scale, colors range from golden-brown to yellow-brown with characteristic chatoyancy (silky luster), trigonal crystal system, indistinct cleavage, and a specific gravity of around 2.64 to 2.71.

Formation & geological history

Formed as a pseudomorph when quartz replaces the original fibrous mineral crocidolite (riebeckite), preserving its fibrous structure over millions of years through hydrothermal processes.

Uses & applications

Widely used in jewelry, decorative items, beads, cabochons, and as a popular specimen for collectors due to its shimmering chatoyant bands.

Geological facts

Tiger's eye is famous for its distinct optical illusion called chatoyancy, where the stone appears to change its brightness or pattern depending on the viewing angle, mimicking a tiger's eye.

Field identification & locations

Easily identified by its golden-brown color and distinctive silky line of light that moves across the surface when turned. Commonly sourced from South Africa, Western Australia, India, and the USA.