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How to identify Hawk's Eye

Silicified Crocidolite (Quartz variety)

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To correctly identify Hawk's Eye (Silicified Crocidolite (Quartz variety)), 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. 1

    Color

    Overall color and any zoning or banding

    Dark blue to bluish-gray, sometimes with greenish or brownish streaks. The blue color is distinct from the golden-brown of Tiger's Eye.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Silky to vitreous, exhibiting a strong chatoyancy.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Fine-grained, fibrous appearance internally, though the surface is smooth when polished.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Massive, fibrous aggregates, pseudomorphing the original crocidolite fibers. Does not form distinct macroscopic crystals.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, as it is a cryptocrystalline quartz. The original crocidolite would have perfect prismatic cleavage, but this is replaced.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found in metamorphosed banded iron formations (BIFs) where crocidolite-rich layers have undergone silicification. These environments are often associated with ancient sedimentary basins.

Key Facts

Hardness
6.5-7 on the Mohs scale (due to quartz)
Specific Gravity
2.64-2.71
Crystal System
Trigonal (for quartz), but pseudomorphs original monoclinic crocidolite structure
Color
Dark blue, bluish-gray, sometimes with greenish or brownish tints
Luster
Silky to vitreous, chatoyant
Transparency
Opaque
Fracture
Conchoidal to splintery
Cleavage
None (for quartz)
Composition
SiO2 (silicon dioxide) with fibrous inclusions of crocidolite (Na2(Fe2+,Mg)3Fe3+2Si8O22(OH)2)

Physical characteristics

  • Crystal Habit: Massive, fibrous aggregates, pseudomorphing original crocidolite
  • Cleavage Type: None (due to quartz replacement)
  • Fracture Type: Conchoidal to splintery
  • Tenacity: Brittle
  • Luster Type: Silky to vitreous

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