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Tiger's Eye

Metamorphic Rock (pseudomorph)

Tiger's Eye

Also known as: Tiger Eye, African Cat's Eye (though distinct from true Cat's Eye chrysoberyl)

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Description

Tiger's Eye is a captivating metamorphic rock characterized by its silky luster and striking chatoyancy, resembling the eye of a tiger. It is a pseudomorph of quartz after crocidolite, meaning quartz has replaced the original crocidolite fibers while retaining their parallel, fibrous structure. The color ranges from golden-yellow to reddish-brown, often with iridescent bands that shift as the stone is moved. This optical phenomenon, known as chatoyancy, is caused by the reflection of light off the minute, parallel fibers of quartz and iron oxides. It is a relatively hard and durable material, making it suitable for various lapidary applications.

How to Identify

Color
Golden-yellow to reddish-brown, often with iridescent bands. Hawk's Eye (blue Tiger's Eye) is blue to bluish-green.
Luster
Silky to vitreous, exhibiting strong chatoyancy.
Texture
Fibrous appearance, even when polished smooth. Can feel cool and smooth to the touch.
Crystal Form
Massive, fibrous aggregates, typically found in veins. Does not form distinct macroscopic crystals.
Cleavage
None, as it is a microcrystalline quartz. The original crocidolite had perfect cleavage, but this is not retained in the quartz pseudomorph.
Geological Environment
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.

Quick Check

  • Color: Golden-yellow to reddish-brown (or blue for Hawk's Eye)
  • Luster: Silky to vitreous, chatoyant
  • Streak: White

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.

Formation

Tiger's Eye forms as a pseudomorph of quartz after crocidolite (a fibrous amphibole mineral, specifically riebeckite). The process involves the infiltration of silica-rich solutions into crocidolite veins. The silica replaces the crocidolite fibers while preserving their original fibrous structure. Oxidation of the iron within the crocidolite (or the replacing silica) gives Tiger's Eye its characteristic golden-yellow to reddish-brown colors. The chatoyancy (cat's-eye effect) is due to the parallel alignment of these preserved fibrous structures.

Usage

Primarily used as a gemstone for cabochons, beads, carvings, and ornamental objects. Its unique chatoyancy makes it popular in jewelry. Historically, it was believed to ward off evil and bring good luck.

Age Distribution

Typically found in Precambrian to Paleozoic age metamorphic terrains.

Where to Find

South Africa

The primary and most significant source of high-quality Tiger's Eye, particularly in the Griqualand West region, Northern Cape Province. Deposits are found in Precambrian banded iron formations.

Australia

Significant deposits are found in Western Australia, particularly in the Hamersley Range, often associated with banded iron formations.

India

Smaller deposits are known, producing material of varying quality.

Myanmar (Burma)

Some occurrences have been reported.

United States

Limited occurrences in states like Arizona and California.

Canada

Minor deposits have been found.

Finding Tips

Look for Metamorphic Terrains

Tiger's Eye is found in regions with ancient metamorphic rocks, particularly those associated with banded iron formations.

Identify Fibrous Structures

Even in rough form, look for a distinct fibrous texture. The chatoyancy might be visible even before polishing.

Observe Color and Luster

The characteristic golden-yellow to reddish-brown color and silky luster are key indicators. Blue varieties (Hawk's Eye) also exist.

Check for Chatoyancy

Rotate the specimen under a light source to observe the moving band of light, which is the hallmark of Tiger's Eye.

Hardness Test

Tiger's Eye is quartz, so it should scratch glass (Mohs hardness 7). This helps differentiate it from softer fibrous minerals.

Similar Rocks

Hawk's Eye

Quartz (pseudomorph after Crocidolite)

Also known as: Blue Tiger's Eye

Pietersite

Chalcedony with embedded Crocidolite fibers

Also known as: Tempest Stone

Cat's Eye Chrysoberyl

Chrysoberyl

Also known as: Cymophane

Scientific Classification

Mineral Class
Silicates (Tectosilicates)
Group
Quartz Group
Crystal System
Trigonal
Chemical Formula
SiO2 (with fibrous inclusions of FeO(OH) and relict crocidolite)
Composition
Silicon dioxide, with the characteristic color and chatoyancy derived from finely fibrous inclusions of iron hydroxides (primarily goethite and limonite) that have replaced the original crocidolite (a sodium-iron amphibole).

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