
mineral
Eagle Eye Stone (Green Tiger's Eye)
Pseudomorph of Quartz after Crocidolite (SiO2 with inclusions)
Hardness: 6.5-7 (Mohs scale); Color: Grayish-green to olive with silky chatoyancy; Luster: Silky to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.64-2.71
- Hardness
- 6
- Color
- Grayish-green to olive with silky chatoyancy
- Luster
- Silky to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Grayish-green to olive with silky chatoyancy; Luster: Silky to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.64-2.71
Formation & geological history
Formed through a pseudomorphic process where silica (quartz) replaces the fibrous mineral crocidolite (blue asbestos) over millions of years. The green coloration typically occurs when the oxidation of iron is incomplete during the change from Hawk's Eye to Tiger's Eye.
Uses & applications
Used primarily for lapidary work, jewelry (cabochons and beads), carvings, and as a metaphysical 'protection' stone for collectors.
Geological facts
This specimen is a variety of chatoyant quartz. It is often considered a transitional phase between Hawk's Eye (blue) and the more common golden-brown Tiger's Eye. When polished, it exhibits a 'cat's eye' effect due to the reflection of light off its internal fiber structures.
Field identification & locations
Identify in the field by its distinctive 'moving' light bands (chatoyancy) and fibrous appearance despite having a smooth, hard surface. It is most commonly found in the Northern Cape Province of South Africa and Western Australia.
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