Rock Identifier
Tiger's Eye (Pseudomorph of Quartz after Crocidolite (SiO2 with iron inclusions)) — metamorphic
metamorphic

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2 with iron inclusions)

Hardness: 6.5–7 (Mohs scale); Color: Golden to red-brown with silky luster; Crystal structure: Trigonal/Fibrous; Cleavage: None; Specific Gravity: 2.64–2.71; Chatoyancy: Distinctive 'cat-eye' optical effect.

Hardness
6
Color
Golden to red-brown with silky luster
Identified More metamorphic

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Physical properties

Hardness: 6.5–7 (Mohs scale); Color: Golden to red-brown with silky luster; Crystal structure: Trigonal/Fibrous; Cleavage: None; Specific Gravity: 2.64–2.71; Chatoyancy: Distinctive 'cat-eye' optical effect.

Formation & geological history

Formed through a metamorphic process where quartz replaces the mineral crocidolite (blue asbestos) while preserving its fibrous structure, often found in Precambrian metamorphic rocks.

Uses & applications

Primarily used in jewelry for cabochons and beads, as well as carvings, decorative ornaments, and widely collected as a metaphysical or healing stone.

Geological facts

This stone is a 'pseudomorph,' meaning 'false form.' It started as a blue mineral (crocidolite) but was completely replaced by silica over millions of years while keeping the original fibers intact.

Field identification & locations

Identify by rotating it under light to see the shimmering bands move (chatoyancy). Commonly found in South Africa, Western Australia, and India. Collectors should look for high-contrast bands and a high polish.