Rock Identifier
Tiger's Eye (Silicon dioxide (SiO2) with fibrous inclusions of Crocidolite (Asbestos) replaced by Quartz) — metamorphic
metamorphic

Tiger's Eye

Silicon dioxide (SiO2) with fibrous inclusions of Crocidolite (Asbestos) replaced by Quartz

Hardness: 6.5–7 Mohs; Color: Golden yellow to silky brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Chatoyancy (cat-eye effect) is its most distinct property.

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

Hardness: 6.5–7 Mohs; Color: Golden yellow to silky brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Chatoyancy (cat-eye effect) is its most distinct property.

Formation & geological history

Formed through the pseudomorphism of crocidolite (blue asbestos) by silica. The iron within the original fibers oxidizes to a golden-brown color during the process. Major deposits date to the Precambrian era.

Uses & applications

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

Geological facts

Tiger's Eye is known for its chatoyancy, an optical effect where light reflects off the parallel fibrous inclusions to create a band of light across the surface. It is considered a 'pseudomorph' because quartz takes the shape of the original mineral.

Field identification & locations

Identify by its distinct golden-brown horizontal banding and silky luster that 'moves' when the stone is tilted. It is most commonly found in South Africa (Northern Cape Province) and Western Australia.