Rock Identifier
Tiger's Eye (Pseudomorph of Quartz after Crocidolite (SiO2)) — mineral
mineral

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2)

Hardness: 7 Mohs; Color: Golden to red-brown; Luster: Silky; Crystal system: Trigonal (fibrous structure); Cleavage: None; Specific Gravity: 2.64-2.71; Notable chatoyancy (cat-eye effect).

Hardness
7 Mohs
Color
Golden to red-brown
Luster
Silky
Identified More mineral
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Physical properties

Hardness: 7 Mohs; Color: Golden to red-brown; Luster: Silky; Crystal system: Trigonal (fibrous structure); Cleavage: None; Specific Gravity: 2.64-2.71; Notable chatoyancy (cat-eye effect).

Formation & geological history

Formed when silica-rich fluids replace fibrous crocidolite (asbestos) crystals over millions of years through a process called pseudomorphism. It is primarily found in Metamorphic rocks, specifically banded iron formations.

Uses & applications

Extensively used in jewelry (beads, cabochons, rings), ornamental carvings, and as a popular pocket stone for collectors.

Geological facts

The chatoyant 'cat-eye' effect is caused by the parallel growth of quartz crystals and altered amphibole fibers. It is considered a protective stone in various cultural traditions.

Field identification & locations

Identified by its distinctive golden-brown bands and the way light reflects off its silky fibrous structure when rotated. It is most abundantly sourced from the Northern Cape Province in South Africa and Western Australia.