Rock Identifier
Tiger's Eye (Pseudomorph of quartz after crocidolite (SiO2)) — metamorphic
metamorphic

Tiger's Eye

Pseudomorph of quartz after crocidolite (SiO2)

Hardness: 7 Mohs; Color: Golden-brown to reddish-brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Chatoyancy (shimmering effect).

Hardness
7 Mohs
Color
Golden-brown to reddish-brown
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 7 Mohs; Color: Golden-brown to reddish-brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Chatoyancy (shimmering effect).

Formation & geological history

Formed when quartz replaces fibrous crocidolite (blue asbestos) via pseudomorphism, preserving the original fibrous structure. Found in iron formations and metamorphic belts.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular collector's gemstone due to its chatoyant properties.

Geological facts

The shimmering 'eye' effect shifts as you rotate the stone. While it starts as blue crocidolite (Hawk's Eye), oxidation of iron within the fibers turns it the golden brown characteristic of Tiger's Eye.

Field identification & locations

Look for distinct parallel golden-yellow and brown bands with a silky sheen. It is most commonly found in South Africa and Western Australia.