
mineral
Green Tiger's Eye
Quartz (SiO2) with fibrous crocidolite inclusions (dyed)
Hardness: 6.5-7 (Mohs); Color: Dark forest green with chatoyant bands; Luster: Silky/Vitreous; Structure: Hexagonal (Trigonal); Cleavage: None; Specific Gravity: 2.64-2.71
- Hardness
- 6
- Color
- Dark forest green with chatoyant bands
- Luster
- Silky/Vitreous
Identified More mineral →
Explore Green Tiger's Eye in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 6.5-7 (Mohs); Color: Dark forest green with chatoyant bands; Luster: Silky/Vitreous; Structure: Hexagonal (Trigonal); Cleavage: None; Specific Gravity: 2.64-2.71
Formation & geological history
Formed when silica-rich fluids replace fibrous crocidolite (asbestos) in iron-rich metamorphic environments. The green color is achieved by chemically dyeing natural golden tiger's eye.
Uses & applications
Primarily used in jewelry for beads, cabochons, and decorative carvings, as well as for metaphysical and collecting purposes.
Geological facts
Tiger's eye exhibits a unique optical phenomenon called chatoyancy, created by the reflection of light off the parallel mineral fibers within the quartz. Naturally occurring green tiger's eye is extremely rare; almost all commercial green specimens are dyed.
Field identification & locations
Identify by rotating the stone in light to observe the moving cat's-eye effect. It is naturally found in South Africa, Australia, and Brazil before processing. Collectors look for sharp, distinct bands of light.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock