
mineral
Limonite Pseudomorph after Pyrite
Limonite (Hydrous iron oxides, FeO(OH)·nH2O) replacing Pyrite (FeS2)
Hardness: 4-5.5 (Mohs scale), Color: Dark brown to yellowish brown, Luster: Dull or earthy, Crystal structure: Isometric (preserving the cubic shape of the original pyrite), Cleavage: None, Specific gravity: 2.7–4.3
- Hardness
- 4-5
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Physical properties
Hardness: 4-5.5 (Mohs scale), Color: Dark brown to yellowish brown, Luster: Dull or earthy, Crystal structure: Isometric (preserving the cubic shape of the original pyrite), Cleavage: None, Specific gravity: 2.7–4.3
Formation & geological history
Formed through oxidation and hydration where water and oxygen chemically transform original pyrite crystals into a mixture of iron oxides (limonite) while preserving the external geometric shape. This is called a pseudomorph (false form).
Uses & applications
Primarily a collector's specimen. Limonite is historically an iron ore and is also used as an earthy pigment (yellow ochre).
Geological facts
Commonly known as 'Prophecy Stones' in metaphysical circles (specifically those from Egypt), these specimens are fascinating because they look like one mineral but are chemically another. They are essentially 'geological ghosts'.
Field identification & locations
Identify in the field by looking for distinct cubic or pyritohedron shapes that are dark brown and non-metallic, unlike true pyrite. They are commonly found in arid desert environments like the White Desert of Egypt or in weathered sedimentary iron-rich beds.
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