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

Red Tiger's Eye

Pseudomorph of Quartz after Crocidolite (Silicon Dioxide: SiO2)

Hardness: 6.5-7 Mohs; Color: Red-brown to mahogany; Luster: Silky to vitreous; Structure: Hexagonal (trigonal); Chatoyancy: Present (cat's eye effect); Specific Gravity: 2.64-2.71

Hardness
6
Color
Red-brown to mahogany
Luster
Silky to vitreous
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Physical properties

Hardness: 6.5-7 Mohs; Color: Red-brown to mahogany; Luster: Silky to vitreous; Structure: Hexagonal (trigonal); Chatoyancy: Present (cat's eye effect); Specific Gravity: 2.64-2.71

Formation & geological history

Formed through the pseudomorphism of blue crocidolite asbestos by silica. The red color is typically produced through natural or artificial heating (oxidation) of common gold tiger's eye, which converts limonite to hematite.

Uses & applications

Primarily used in jewelry (beads, cabochons), metaphysical practices, and ornamental carvings.

Geological facts

Also known as Ox's Eye or Bull's Eye. The trademark chatoyancy is caused by the light reflecting off the parallel fibrous structure of the mineral. While it can occur naturally through geothermal heat, most red tiger's eye on the market is heat-treated.

Field identification & locations

Identify in the field by its distinct chatoyant 'shimmer' when rotated under light and its heavy fibrous banding. Major deposits are found in South Africa, Western Australia, India, and Namibia.