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

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (Silicon Dioxide: SiO2)

Hardness: 6.5-7 (Mohs). Color: Golden yellow to deep brown with silky chatoyant bands. Luster: Silky. Crystal structure: Trigonal/Fibrous. Cleavage: None. Specific gravity: 2.64-2.71.

Hardness
6
Color
Golden yellow to deep brown with silky chatoyant bands
Luster
Silky
Identified More metamorphic

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Physical properties

Hardness: 6.5-7 (Mohs). Color: Golden yellow to deep brown with silky chatoyant bands. Luster: Silky. Crystal structure: Trigonal/Fibrous. Cleavage: None. Specific gravity: 2.64-2.71.

Formation & geological history

Formed through a metamorphic process known as pseudomorphism, where silica replaces fibrous crocidolite (asbestos) while maintaining the original fibrous structure. Most deposits are found in Precambrian iron formations.

Uses & applications

Primarily used in jewelry (beads, cabochons), ornamental carvings, and as a popular semi-precious stone for collectors emphasizing its chatoyancy.

Geological facts

The unique 'shimmer' is called chatoyancy or the 'cat-eye effect.' Historically, it was worn by Roman soldiers in battle for protection and was once valued more highly than gold before large deposits were found in South Africa.

Field identification & locations

Identify in the field by its distinct golden-brown bands that seem to move when the stone is rotated under a light source. Commonly found in South Africa, Australia, Burma, and India. Look for silky luster and fibrous texture in raw specimens.