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 scale); Color: Golden yellow to brown/black bands; Luster: Silky; Crystal structure: Trigonal (fibrous texture); Cleavage: None; Specific gravity: 2.64-2.71.

Hardness
6
Color
Golden yellow to brown/black bands
Luster
Silky
Identified More metamorphic

Identify your own rocks.

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

Physical properties

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

Formation & geological history

Formed through the metamorphic process where quartz replaces the fibrous mineral crocidolite (blue asbestos) while retaining the original fibrous structure. Most deposits are Proterozoic in age (approx. 2 billion years old).

Uses & applications

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

Geological facts

Exhibits chatoyancy (the 'cat's eye' effect) due to the parallel orientation of internal fibers. Historically, it was worn by Roman soldiers in battle for protection and courage.

Field identification & locations

Identify by its alternating bands of gold and dark brown and its distinct silky shimmering effect when tilted under light. Commonly found in South Africa (Griquatown) and Western Australia.