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-brown to yellow-gold; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Notable for its chatoyancy or 'cat's eye' effect.

Hardness
7 (Mohs)
Color
Golden-brown to yellow-gold
Luster
Silky
Identified More mineral

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7 (Mohs); Color: Golden-brown to yellow-gold; Luster: Silky; Crystal structure: Trigonal (fibrous); Cleavage: None; Specific Gravity: 2.64-2.71; Notable for its chatoyancy or 'cat's eye' effect.

Formation & geological history

Formed through a pseudomorphic process where silica (Quartz) replaces the fibrous mineral Crocidolite while retaining the original fibrous structure. Most deposits are found in Precambrian iron formations around 2 billion years old.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, lapidary arts, and as a popular specimen for crystal collectors.

Geological facts

It is a chatoyant gemstone that exhibits a unique silky luster due to the parallel growth of quartz crystals and altered amphibole fibers. 'Blue Tiger\'s Eye' is known as Hawk\'s Eye and represents a stage where the asbestos fibers have not yet been oxidized by iron.

Field identification & locations

Identify by its distinctive bands of gold and brown and its optical chatoyancy when rotated under light. Major locations include South Africa (Northern Cape), Australia, Myanmar, and Namibia.