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 to red-brown; Luster: Silky; Structure: Trigonal (fibrous); Specific Gravity: 2.64-2.71; Notable for chatoyancy.

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

Hardness: 7 Mohs; Color: Golden to red-brown; Luster: Silky; Structure: Trigonal (fibrous); Specific Gravity: 2.64-2.71; Notable for chatoyancy.

Formation & geological history

Formed through the pseudomorphism of blue asbestos (crocidolite) fibers by silica. As the iron oxidizes, it turns the original blue mineral to gold or brown. Primary sources date back to the Precambrian era.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular collectible gemstone due to its chatoyant effect.

Geological facts

It is a 'pseudomorph', meaning one mineral has replaced another while retaining the original mineral's shape. The name comes from its resemblance to the eye of a tiger or cat.

Field identification & locations

Identify by its distinct golden-brown banded pattern and silky 'moving' light effect when rotated. Commonly found in South Africa and Western Australia. Collectors look for sharp, distinct chatoyancy.