
mineral
Tiger's Eye
Silicon Dioxide (SiO2) - Pseudomorph of Quartz after Crocidolite
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Golden to red-brown. Luster: Silky. Crystal system: Trigonal (microcrystalline quartz aggregate). Cleavage: None. Specific gravity: 2.64-2.71. Displays strong chatoyancy (cat's eye effect).
- Hardness
- 7 on Mohs scale
- Color
- Golden to red-brown
- Luster
- Silky
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Physical properties
Hardness: 7 on Mohs scale. Color: Golden to red-brown. Luster: Silky. Crystal system: Trigonal (microcrystalline quartz aggregate). Cleavage: None. Specific gravity: 2.64-2.71. Displays strong chatoyancy (cat's eye effect).
Formation & geological history
Formed when quartz replaces fibrous crocidolite (blue asbestos) amphibole fibers through a process called pseudomorphism, while preserving the original fibrous structure. Highly common in iron-rich metamorphic and sedimentary formations.
Uses & applications
Widely used in jewelry (beads, cabochons, carved ornaments), decorative objects, metaphysical healing crystals, and lapidary collections.
Geological facts
Tiger's eye is famous for its chatoyant optical effect caused by parallel fibers of quartz intergrown with amphibole fibers or iron oxide inclusions. When heat-treated, brown/golden tiger's eye turns deep red.
Field identification & locations
Identified by its distinctive silky, golden-brown banding and silky shimmer when rotated under light. Major commercial sources include South Africa, Western Australia, India, Brazil, and Namibia.
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