
gemstone
Tiger's Eye
Quartz pseudomorph after crocidolite (SiO2)
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale; Color: Golden-brown, yellow-brown, with bands of contrasting light; Luster: Silky to vitreous; Crystal structure: Trigonal (microcrystalline quartz, pseudomorphous); Specific gravity: 2.64-2.71
- Hardness
- 7 on the Mohs scale
- Color
- Golden-brown, yellow-brown, with bands of contrasting light
- Luster
- Silky to vitreous
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Physical properties
Hardness: 7 on the Mohs scale; Color: Golden-brown, yellow-brown, with bands of contrasting light; Luster: Silky to vitreous; Crystal structure: Trigonal (microcrystalline quartz, pseudomorphous); Specific gravity: 2.64-2.71
Formation & geological history
Formed as a metamorphic replacement when quartz progressively replaces the blue asbestos mineral crocidolite, preserving its fibrous structure.
Uses & applications
Widely used in jewelry, cabochons, beads, decorative carvings, and as a popular collector mineral.
Geological facts
Tiger's eye exhibits a distinct chatoyancy (cat's-eye effect) caused by the parallel fibrous structure of the original crocidolite crystals reflecting light.
Field identification & locations
Easily identified by its characteristic golden-brown stripes and silky chatoyancy. Primarily sourced from South Africa and Western Australia; finding it in North Carolina would indicate it was purchased or transported, as it is geologically foreign to the local sedimentary and metamorphic formations of the region.
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