How to identify Tiger's Eye
Tiger's Eye
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Open the appTo correctly identify Tiger's Eye (Tiger's Eye), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Golden-yellow to reddish-brown, often with iridescent bands. Hawk's Eye (blue Tiger's Eye) is blue to bluish-green.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Silky to vitreous, exhibiting strong chatoyancy.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Fibrous appearance, even when polished smooth. Can feel cool and smooth to the touch.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Massive, fibrous aggregates, typically found in veins. Does not form distinct macroscopic crystals.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, as it is a microcrystalline quartz. The original crocidolite had perfect cleavage, but this is not retained in the quartz pseudomorph.
- 6
Geological Environment
The rock formation and setting where it occurs
Formed in metamorphic terrains where crocidolite-rich rocks (often associated with banded iron formations) have undergone silicification. Typically found in veins or seams within these host rocks.
Key Facts
- Hardness
- 7 (Mohs scale)
- Specific Gravity
- 2.64 - 2.71
- Crystal System
- Trigonal (as quartz)
- Color
- Golden-yellow, golden-brown, reddish-brown; blue (Hawk's Eye)
- Luster
- Silky, vitreous
- Transparency
- Opaque to translucent
- Fracture
- Conchoidal to splintery
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2) with inclusions of iron oxides (limonite, goethite) and relict crocidolite fibers.
Physical characteristics
- Crystal Habit: Massive, fibrous aggregates, pseudomorph after crocidolite.
- Cleavage Type: None (as quartz). Original crocidolite had perfect cleavage.
- Fracture Type: Conchoidal to splintery.
- Tenacity: Brittle.
- Luster Type: Silky to vitreous, chatoyant.
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