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 brown with chatoyant bands; Luster: Silky; Crystal structure: Trigonal (fibrous texture); Cleavage: None; Specific Gravity: 2.64-2.71.

Hardness
6
Color
Golden yellow to brown with chatoyant bands
Luster
Silky
Identified More metamorphic

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Golden yellow to brown with chatoyant bands; Luster: Silky; Crystal structure: Trigonal (fibrous texture); Cleavage: None; Specific Gravity: 2.64-2.71.

Formation & geological history

Formed through the pseudomorphism of crocidolite asbestos fibers by chalcedony quartz. Heat and pressure during tectonic movements replace the blue asbestos with quartz and iron oxides while maintaining the fibrous structure. Primarily found in Precambrian rocks.

Uses & applications

Predominantly used as a gemstone for jewelry (cabochons, beads), decorative carvings, and as a popular specimen for rock collectors.

Geological facts

The optical effect seen in Tiger's Eye is called chatoyancy, or the 'cat's-eye effect.' It was historically worn as an amulet against curses and bad luck. The largest deposits are in the Griquatown area of South Africa.

Field identification & locations

Identified in the field by its distinct parallel bands of golden-brown color and the way light reflects off the fibrous surface as the stone is turned (chatoyancy). Common locations include South Africa, Australia, Burma, and India.