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Tiger's Eye

Metamorphic Rock (pseudomorph of Quartz after Crocidolite)

Tiger's Eye (a variety of Chalcedony)

Also known as: Tiger Eye, African Tiger's Eye

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Description

Tiger's Eye is a captivating variety of chalcedony, a cryptocrystalline form of silica, renowned for its striking chatoyancy, an optical phenomenon resembling the slit pupil of a cat's or tiger's eye. This effect is caused by the parallel intergrowth of quartz fibers and altered amphibole minerals, primarily crocidolite, which have been replaced by silica and stained by iron oxides. The color typically ranges from golden-yellow to reddish-brown, often with iridescent bands that shift with light. It is a pseudomorph, meaning one mineral (quartz) has replaced another (crocidolite) while preserving the original mineral's external form.

How to Identify

Color
Golden-yellow to reddish-brown, often with iridescent bands.
Luster
Silky to vitreous.
Texture
Fibrous appearance, often visible on polished surfaces.
Crystal Form
Cryptocrystalline, typically massive with a fibrous structure.
Cleavage
None, due to its cryptocrystalline nature.
Geological Environment
Typically found in low-grade metamorphic rocks, often associated with serpentinites or other ultramafic rocks where crocidolite forms. It occurs 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 aggregates of quartz).
  • Color: Golden-yellow, golden-brown, reddish-brown.
  • Luster: Silky to vitreous.
  • Transparency: Opaque to translucent.
  • Fracture: Conchoidal to splintery.
  • Cleavage: None.
  • Composition: Silicon dioxide (SiO2) with inclusions of iron oxides.

Quick Check

  • Color: Golden-yellow to reddish-brown with iridescent bands.
  • Luster: Silky to vitreous.
  • Streak: White.

Physical Characteristics

  • Crystal Habit: Massive, fibrous aggregates.
  • Cleavage Type: None.
  • Fracture Type: Conchoidal to splintery.
  • Tenacity: Brittle.
  • Luster Type: Silky (due to fibrous structure) to vitreous (on broken surfaces).

Formation

Tiger's Eye forms as a pseudomorph of quartz after the fibrous mineral crocidolite (a type of asbestos). The original crocidolite fibers are replaced by silica (quartz) while retaining the fibrous structure. The characteristic golden-brown color and chatoyancy are due to the presence of iron oxides (limonite) that stain the quartz fibers, often after the oxidation of the original crocidolite. This process typically occurs in low-grade metamorphic environments.

Usage

Primarily used as a gemstone for jewelry (cabochons, beads, carvings), ornamental objects, and decorative items. Its unique chatoyancy makes it highly sought after.

Age Distribution

Formed in various geological periods, often associated with Precambrian to Cenozoic metamorphic events.

Where to Find

South Africa

The primary and most significant source, particularly in the Griqualand West region, where vast deposits are found in banded iron formations.

Australia

Western Australia has notable deposits, often producing material with a slightly different color range.

India

Smaller deposits are found, contributing to the global supply.

Myanmar (Burma)

Known for some occurrences, though less prominent than South Africa.

United States

Limited occurrences in states like California and Arizona.

Finding Tips

Look for Chatoyancy

The most distinctive feature is its chatoyancy. Rotate the specimen under a light source to observe the moving band of light.

Examine Color and Pattern

Observe the characteristic golden-yellow to reddish-brown colors and the parallel fibrous bands.

Check Hardness

Tiger's Eye has a Mohs hardness of 6.5-7, which can be tested with common tools (e.g., it will scratch glass).

Consider Geological Context

If collecting in the field, look for areas with metamorphic rocks, especially those associated with banded iron formations or serpentinites.

Safety Precaution: Crocidolite

While Tiger's Eye itself is quartz and generally safe, its formation involves the replacement of crocidolite (a type of asbestos). Unpolished, raw specimens, especially those with visible blue fibers (Hawk's Eye), might contain residual crocidolite. Avoid inhaling dust from cutting or grinding raw material without proper respiratory protection. Polished Tiger's Eye is considered safe as the asbestos fibers are encapsulated by quartz.

Similar Rocks

Hawk's Eye

Quartz (variety Chalcedony, pseudomorph after Crocidolite)

Also known as: Blue Tiger's Eye

Cat's Eye Chrysoberyl

Chrysoberyl

Also known as: Cymophane

Pietersite

Chalcedony with embedded Crocidolite fibers

Also known as: Tempest Stone

Scientific Classification

Mineral Class
Silicates (Tectosilicates)
Group
Quartz Group (Chalcedony variety)
Crystal System
Trigonal (microcrystalline quartz)
Chemical Formula
SiO2 (with FeOOH inclusions)
Composition
Silicon dioxide, with iron oxide (limonite) inclusions responsible for color and chatoyancy, formed as a pseudomorph after crocidolite.

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