
mineral
Red Tiger's Eye
SiO2 (Silicon Dioxide with iron inclusions)
AI-generated identification · may be incorrectHardness: 7 Mohs; Color: Brownish-red to deep red with chatoyancy; Luster: Silky; Crystal structure: Trigonal (fibrous aggregate); Specific Gravity: 2.64-2.71
- Hardness
- 7 Mohs
- Color
- Brownish-red to deep red with chatoyancy
- Luster
- Silky
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Physical properties
Hardness: 7 Mohs; Color: Brownish-red to deep red with chatoyancy; Luster: Silky; Crystal structure: Trigonal (fibrous aggregate); Specific Gravity: 2.64-2.71
Formation & geological history
Formed through the pseudomorphism of crocidolite fibers by quartz. The red color is typically a result of heating (natural or artificial) which oxidizes the iron content (limonite) into hematite.
Uses & applications
Predominantly used for lapidary purposes including jewelry (cabochons, beads), decorative carvings, and as a popular specimen for metaphysical collectors.
Geological facts
Also known as Bull's Eye. It exhibits a unique optical effect called chatoyancy, which creates a shimmering 'cat's eye' band that moves across the stone as it is rotated in light.
Field identification & locations
Identify by the distinctive silky luster and moving bands of light (chatoyancy). It is often found in banded iron formations. Key locations include South Africa, Australia, and Brazil.
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Epidote
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