How to identify Tiger's Eye
Tiger's Eye (a variety of Chalcedony, which is cryptocrystalline Quartz)
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Open the appTo correctly identify Tiger's Eye (Tiger's Eye (a variety of Chalcedony, which is cryptocrystalline Quartz)), 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-brown, yellow-brown, reddish-brown, sometimes blue (Hawk's Eye). The colors are typically banded or streaked.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Silky to vitreous, especially on polished surfaces, due to chatoyancy.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Fibrous internal structure, often visible as parallel lines or bands. Smooth to the touch when polished.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Massive, fibrous aggregates. Does not form macroscopic crystals.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, as it is cryptocrystalline quartz.
- 6
Geological Environment
The rock formation and setting where it occurs
Typically found in metamorphosed ultramafic rocks, often associated with serpentinite bodies, where crocidolite asbestos veins have been replaced by quartz. It forms in veins or seams within these host rocks.
Key Facts
- Hardness
- 6.5-7 on the Mohs scale
- Specific Gravity
- 2.64 - 2.71
- Crystal System
- Trigonal (cryptocrystalline)
- Color
- Golden-brown, yellow-brown, reddish-brown, blue (Hawk's Eye)
- Luster
- Silky to vitreous
- Transparency
- Opaque to translucent
- Fracture
- Conchoidal to splintery
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2) with inclusions of limonite and relict crocidolite fibers
Physical characteristics
- Crystal Habit: Massive, fibrous aggregates, pseudomorph after crocidolite
- Cleavage Type: None
- Fracture Type: Conchoidal to splintery
- Tenacity: Brittle
- Luster Type: Silky (chatoyant) to vitreous
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