Rock Identifier
Tiger's Eye (Pseudomorph of Quartz after Crocidolite (SiO2 with inclusions of Iron Oxide)) — Metamorphic
Metamorphic

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2 with inclusions of Iron Oxide)

Hardness: 6.5-7 (Mohs); Color: Golden to red-brown with silky luster; Crystal system: Trigonal/Fibrous; No cleavage; Specific gravity: 2.64-2.71; Notable for chatoyancy (cat's eye effect).

Hardness
6
Color
Golden to red-brown with silky luster
Identified More metamorphic
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Physical properties

Hardness: 6.5-7 (Mohs); Color: Golden to red-brown with silky luster; Crystal system: Trigonal/Fibrous; No cleavage; Specific gravity: 2.64-2.71; Notable for chatoyancy (cat's eye effect).

Formation & geological history

Formed through the pseudomorphism of crocidolite (asbestos). Over time, quartz replaces the asbestos fibers while retaining the original fibrous structure. The golden color comes from oxidized iron. Most deposits are billions of years old.

Uses & applications

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

Geological facts

The unique 'shimmer' of Tiger's Eye is called chatoyancy. If the iron is not oxidized and remains blue, the stone is called 'Hawk's Eye'. It is the 9th wedding anniversary stone.

Field identification & locations

Identify by its distinct golden-brown banding and the way light reflects off the fibrous inclusions when tilted. It is most commonly found in South Africa and Western Australia.