Rock Identifier
Tiger's Eye (SiO2 (Quartz pseudomorph after crocidolite)) — mineral
mineral

Tiger's Eye

SiO2 (Quartz pseudomorph after crocidolite)

Hardness: 7 on Mohs scale. Color: Golden to red-brown, with silky luster and distinct chatoyancy (cat's-eye effect). Hexagonal crystal system (microcrystalline).

Hardness
7 on Mohs scale
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale. Color: Golden to red-brown, with silky luster and distinct chatoyancy (cat's-eye effect). Hexagonal crystal system (microcrystalline).

Formation & geological history

Formed when quartz replaces fibrous blue crocidolite (asbestos) amphibole minerals through a process called pseudomorphism, retaining the fibrous structure that causes chatoyancy.

Uses & applications

Popular gemstone used for jewelry, beads, cabochons, carvings, decorative polished stones, and ornamental items.

Geological facts

The chatoyant effect seen in Tiger's Eye is caused by parallel intergrowths of quartz crystals and altered amphibole fibers that reflect light in a silky band.

Field identification & locations

Identified by its distinctive golden-brown banded color and shimmering chatoyant luster when polished. Commonly found in South Africa, Australia, India, and Brazil.