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; Color: Golden-brown to yellow with chatoyancy; Luster: Silky; Crystal system: Trigonal/Fibrous; Specific Gravity: 2.64-2.71

Hardness
6
Color
Golden-brown to yellow with chatoyancy
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 6.5-7 Mohs; Color: Golden-brown to yellow with chatoyancy; Luster: Silky; Crystal system: Trigonal/Fibrous; Specific Gravity: 2.64-2.71

Formation & geological history

Formed through a process called pseudomorphism, where silica replaces existing crocidolite (asbestos) fibers while preserving the fibrous structure. It is typically found in metamorphic formations associated with iron-bearing sedimentary rocks.

Uses & applications

Used primarily in jewelry as cabochons, beads, and carvings. Also popular as a metaphysical/healing stone and for lapidary collections.

Geological facts

The characteristic shimmer is called chatoyancy, or the 'cat's eye' effect. If the iron in the stone is oxidized through heating, it turns red (Red Tiger's Eye). If the material is not fully oxidized, it remains blue (Hawk's Eye).

Field identification & locations

Identify by its distinct golden-brown bands and the way the reflective light moves across its surface when tilted. Major deposits are found in South Africa, Australia, and Namibia.