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

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2 with iron oxides)

Hardness: 6.5-7; Color: Golden yellow to deep brownish-red with distinct chatoyant bands; Luster: Silky; Crystal structure: Trigonal; Fracture: Fibrous

Hardness
6
Luster
Silky
Identified More metamorphic
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Physical properties

Hardness: 6.5-7; Color: Golden yellow to deep brownish-red with distinct chatoyant bands; Luster: Silky; Crystal structure: Trigonal; Fracture: Fibrous

Formation & geological history

Formed when quartz replaces fibrous crocidolite (asbestos) through a process of pseudomorphism, retaining the original fibrous structure. Most deposits are Proterozoic in age.

Uses & applications

Predominantly used as a semi-precious gemstone in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for collectors.

Geological facts

The chatoyancy (cat's eye effect) is caused by the parallel reflection of light off the internal fibrous structure. It is often associated with the 'Solar Plexus' chakra in metaphysical traditions.

Field identification & locations

Look for a distinct 'shimmer' or moving band of light when rotating the stone under a light source. Commonly found in South Africa, Western Australia, India, and Myanmar.