How to identify Goethite
α-FeO(OH)
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Open the appTo correctly identify Goethite (α-FeO(OH)), 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
Color
Overall color and any zoning or banding
Yellowish-brown, reddish-brown, dark brown to black. Often appears rusty.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Adamantine to dull, silky (fibrous varieties), earthy (massive varieties).
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Earthy, fibrous, botryoidal, stalactitic, reniform, or massive.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Orthorhombic. Crystals are typically prismatic, acicular (needle-like), or tabular, often striated. More commonly found in massive, botryoidal, reniform, or stalactitic aggregates.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Perfect on {010}, but rarely observed in massive or fibrous forms.
- 6
Geological Environment
The rock formation and setting where it occurs
Oxidation zones of iron ore deposits, gossans, lateritic soils, bogs, swamps, sedimentary iron formations, and as a weathering product of iron-bearing silicates and sulfides.
Key Facts
- Hardness
- 5.0-5.5 (Mohs scale)
- Specific Gravity
- 3.3-4.3 (variable depending on porosity and impurities)
- Crystal System
- Orthorhombic
- Color
- Yellowish-brown, reddish-brown, dark brown to black
- Luster
- Adamantine, submetallic, silky, dull, earthy
- Transparency
- Opaque
- Fracture
- Uneven to subconchoidal
- Cleavage
- Perfect on {010}, but rarely observed
- Composition
- Iron oxyhydroxide (α-FeO(OH))
Physical characteristics
- Crystal Habit: Prismatic, acicular, tabular, massive, botryoidal, reniform, stalactitic, fibrous, earthy
- Cleavage Type: Perfect on {010}, but often not apparent in massive forms
- Fracture Type: Uneven to subconchoidal
- Tenacity: Brittle
- Luster Type: Adamantine to dull, silky, earthy
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