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

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2)

Hardness: 6.5-7.0 (Mohs); Color: Golden to red-brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Chatoyancy (cat's-eye effect).

Hardness
6
Color
Golden to red-brown
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 6.5-7.0 (Mohs); Color: Golden to red-brown; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Chatoyancy (cat's-eye effect).

Formation & geological history

Formed when quartz replaces the mineral crocidolite (blue asbestos) through a process of pseudomorphism, typically in iron formations within metamorphic rock environments. Most specimens are over 2 billion years old.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular collectible stone in metaphysical practices.

Geological facts

The characteristic silky luster comes from the parallel growth of quartz crystals and altered amphibole fibers. A blue variety exists called Hawk's Eye, and a heat-treated red variety is known as Bull's Eye.

Field identification & locations

Identify by looking for moving bands of light (chatoyancy) when the stone is rotated under a light source. Commonly found in South Africa, Western Australia, India, and Burma.