Rock Identifier
Tiger's Eye (Pseudomorph of Quartz after Crocidolite (SiO2)) — metamorphic
metamorphic

Tiger's Eye

Pseudomorph of Quartz after Crocidolite (SiO2)

Hardness: 7 (Mohs scale), Color: Golden yellow to brown, Luster: Silky/Vitreous, Structure: Fibrous, Cleavage: None, Specific Gravity: 2.64-2.71

Identified More metamorphic

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Physical properties

Hardness: 7 (Mohs scale), Color: Golden yellow to brown, Luster: Silky/Vitreous, Structure: Fibrous, Cleavage: None, Specific Gravity: 2.64-2.71

Formation & geological history

Formed through a metamorphic process where quartz replaces the fibers of the mineral crocidolite (blue asbestos). It typically forms in Precambrian banded iron formations through the infiltration of silica-rich fluids.

Uses & applications

Predominantly used for jewelry, lapidary arts, carvings, and as a popular semi-precious gemstone for decorative objects and mineral collecting.

Geological facts

It exhibits chatoyancy, the 'cat-eye' effect, caused by the fibrous structure within the stone reflecting light. If the quartz replacement is incomplete, it may remain blue, known as Hawk's Eye.

Field identification & locations

Identify in the field by its distinct yellow-gold and brown bands and its unique chatoyant shimmer when rotated under light. Common locations include South Africa, Western Australia, and Namibia.