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 yellow to brown with chatoyant bands; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71

Hardness
6
Color
Golden yellow to brown with chatoyant bands
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 6.5-7 Mohs; Color: Golden yellow to brown with chatoyant bands; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71

Formation & geological history

Formed through the pseudomorphism of crocidolite (blue asbestos) fiber by silica. As quartz replaces the fibers, it retains the fibrous structure, creating chatoyancy. Most deposits are found in Precambrian banded iron formations.

Uses & applications

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

Geological facts

The 'eye' effect is known as chatoyancy. It is believed by some cultures to provide protection and clarity. It is the anniversary gemstone for the 9th year of marriage.

Field identification & locations

Identify by moving the stone under a light source to observe the shifting 'cat-eye' bands. Commonly found in South Africa (Northern Cape), Australia, and Namibia. Collectors look for high luster and straight, sharp banding.