Rock Identifier
Tiger's Eye (Pseudomorph of Quartz after Crocidolite (SiO2 with iron oxide inclusions)) — metamorphic
metamorphic

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2 with iron oxide inclusions)

Hardness: 6.5-7.0 (Mohs); Color: Golden yellow to silky brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific gravity: 2.64-2.71.

Hardness
6
Color
Golden yellow to silky brown
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 6.5-7.0 (Mohs); Color: Golden yellow to silky brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific gravity: 2.64-2.71.

Formation & geological history

Formed when quartz replaces the fibrous mineral crocidolite (blue asbestos) through a process of silicone dioxide infiltration, while maintaining the original fibrous structure. Most deposits are Proterozoic in age.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular meditation or 'healing' stone in metaphysical circles.

Geological facts

The characteristic 'cat's eye' effect is called chatoyancy, caused by the reflection of light off the parallel fibrous inclusions. When heated, the iron oxides turn red, creating 'Red Tiger\'s Eye'.

Field identification & locations

Identified by its signature bands of golden yellow and dark brown with a silky, moving shimmer when rotated. Major sources include South Africa, Western Australia, India, and Burma.