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How to identify Iridescent Goethite

Goethite (α-FeOOH)

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To correctly identify Iridescent Goethite (Goethite (α-FeOOH)), 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

    Base color is dark brown to black, but the surface exhibits strong metallic iridescence with colors like blue, green, gold, purple, and red.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Submetallic to metallic, with a distinct iridescent sheen on the surface.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Often botryoidal, stalactitic, reniform, or massive. Surfaces can be smooth or mammillary.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically forms in radiating fibrous aggregates, botryoidal, stalactitic, or reniform masses. Individual crystals are rare and usually acicular or prismatic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect on {010}, but rarely observed due to its typical massive or fibrous habit.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in the oxidized zones of iron ore deposits, gossans, lateritic soils, and as a weathering product of iron-rich minerals. It can also form in bog iron deposits and hydrothermal veins.

Key Facts

Hardness
5 - 5.5 on the Mohs scale.
Specific Gravity
3.3 - 4.3, typically around 4.0.
Crystal System
Orthorhombic.
Color
Dark brown to black, with iridescent surface colors.
Luster
Submetallic to metallic, with strong iridescence.
Transparency
Opaque.
Fracture
Uneven to splintery.
Cleavage
Perfect on {010}, but rarely observed.
Composition
Hydrous iron oxide (α-FeOOH).

Physical characteristics

  • Crystal Habit: Typically botryoidal, stalactitic, reniform, massive, fibrous, or acicular. Rarely forms distinct prismatic crystals.
  • Cleavage Type: Perfect on one direction ({010}), but often obscured by its common habits.
  • Fracture Type: Uneven to splintery.
  • Tenacity: Brittle.
  • Luster Type: Submetallic to metallic, with a characteristic iridescent sheen.

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