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; Color: Golden yellow to brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Notable for chatoyancy.

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

Hardness: 6.5-7 Mohs; Color: Golden yellow to brown; Luster: Silky; Crystal structure: Trigonal/Fibrous; Specific Gravity: 2.64-2.71; Notable for chatoyancy.

Formation & geological history

Formed through the pseudomorphism of crocidolite (asbestos) by silica. The original fibrous structure is preserved while being replaced by quartz, with iron oxidation producing the golden-brown hues. Most deposits are found in Precambrian rock units.

Uses & applications

Primarily used as a gemstone in jewelry (beads, cabochons), carvings, and ornamental objects. It is also a popular specimen for crystal healing collectors.

Geological facts

Tiger's Eye exhibits an optical effect known as chatoyancy or the 'cat\'s eye effect,' caused by the reflection of light off the parallel mineral fibers. If the stone is heated, it turns red (Red Tiger\'s Eye), and if naturally oxidized differently, it may remain blue (Hawk\'s Eye).

Field identification & locations

Identify by its characteristic moving bands of light (silkiness) and yellow/gold/brown color scheme. It is most commonly found in South Africa, Australia, India, and Burma. Collectors look for sharp, clean chatoyancy without dull spots.