Rock Identifier
Tiger's Eye (Pseudomorph of quartz after crocidolite (SiO2 with iron inclusions)) — metamorphic
metamorphic

Tiger's Eye

Pseudomorph of quartz after crocidolite (SiO2 with iron inclusions)

Hardness: 6.5–7 (Mohs scale); Color: Golden to reddish-brown; Luster: Silky to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Chatoyancy: Strong (cat's eye effect).

Hardness
6
Color
Golden to reddish-brown
Luster
Silky to vitreous
Identified More metamorphic

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Physical properties

Hardness: 6.5–7 (Mohs scale); Color: Golden to reddish-brown; Luster: Silky to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Chatoyancy: Strong (cat's eye effect).

Formation & geological history

Formed through the pseudomorphism of crocidolite (blue asbestos) by silica. Iron from the original mineral oxidizes to create the signature golden-brown color. Predominant in Precambrian formations.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular semi-precious stone for gemstone collectors.

Geological facts

Roman soldiers wore engraved tiger's eye for protection in battle; it is known for its chatoyancy, an optical effect caused by the parallel orientation of mineral fibers.

Field identification & locations

Identify in the field by its distinctive golden-brown sheen and 'cat's eye' bands that move as the stone is tilted. Heavily mined in South Africa and Western Australia.