
mineral
Goethite pseudomorph after Pyrite
Goethite (FeO(OH)) pseudomorph after Pyrite (FeS2)
AI-generated identification · may be incorrectForm: Cuboidal or pyritohedral crystal habit. Hardness: 5-5.5 (Goethite) vs original Pyrite. Color: Dark brown to blackish. Luster: Dull to sub-metallic. Crystal Structure: Orthorhombic. Specific Gravity: 3.3-4.3.
- Hardness
- 5-5
- Color
- Dark brown to blackish
- Luster
- Dull to sub-metallic
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Physical properties
Form: Cuboidal or pyritohedral crystal habit. Hardness: 5-5.5 (Goethite) vs original Pyrite. Color: Dark brown to blackish. Luster: Dull to sub-metallic. Crystal Structure: Orthorhombic. Specific Gravity: 3.3-4.3.
Formation & geological history
This specimen is a pseudomorph, where the mineral Goethite has replaced the original Pyrite crystal structure through chemical weathering and oxidation while maintaining the original crystal shape. Often found in sedimentary or metamorphic host rocks.
Uses & applications
Primarily for mineral collecting and educational purposes. Historically, Goethite is an ore of iron.
Geological facts
These are often nicknamed 'Prophecy Stones' in a metaphysical context or 'Limonite/Goethite cubes' in geology. The term pseudomorph literally means 'false form'.
Field identification & locations
Identify by the distinct cubic or multi-faceted pyritohedral shape combined with a dark brown, rusty oxidation color and lack of metallic brassy luster characteristic of fresh pyrite. Commonly found in desert environments or weathering outcrops.
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