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

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2)

Hardness: 6.5–7 (Mohs scale); Color: Golden yellow to deep brown; Luster: Silky; Crystal Structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64–2.71

Hardness
6
Color
Golden yellow to deep brown
Luster
Silky
Identified More metamorphic

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 6.5–7 (Mohs scale); Color: Golden yellow to deep brown; Luster: Silky; Crystal Structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64–2.71

Formation & geological history

Formed through the metamorphic transformation of fibrous blue crocidolite asbestos by silica. The silica replaces the asbestos fibers while maintaining the original fibrous structure. Most deposits are found in Precambrian iron formations.

Uses & applications

Primarily used for jewelry (cabochons, beads), decorative carvings, ornamental handles, and as a popular specimen for crystal healing and metaphysical collections.

Geological facts

It exhibits a unique optical phenomenon called 'chatoyancy' or the 'cat-eye effect,' caused by the reflection of light off the internal fibrous structure. Roman soldiers carried it for protection during battle.

Field identification & locations

Identify in the field by its distinct alternating bands of yellow and brown and its chatoyant 'shifting' light effect when rotated. Common locations include South Africa (Northern Cape), Western Australia, India, and Burma.