
sedimentary
Yellow Ocherous Siltstone (Limonitic Shale)
Limonitic Siltstone / Goethite-rich Sedimentary Rock
AI-generated identification · may be incorrectHardness: 2-4 (Mohs scale); Color: Yellow to brownish-orange; Luster: Dull, earthy; Crystal structure: Microcrystalline/Amorphous; Cleavage: None (conchoidal or irregular fracture); Specific gravity: 2.7-4.3 influenced by iron content
- Hardness
- 2-4 (Mohs scale)
- Color
- Yellow to brownish-orange
- Luster
- Dull, earthy
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Physical properties
Hardness: 2-4 (Mohs scale); Color: Yellow to brownish-orange; Luster: Dull, earthy; Crystal structure: Microcrystalline/Amorphous; Cleavage: None (conchoidal or irregular fracture); Specific gravity: 2.7-4.3 influenced by iron content
Formation & geological history
Formed through the accumulation of fine-grained silt and clay in low-energy environments like lake beds or floodplains, followed by the secondary oxidation and hydration of iron minerals (limonitization) within the sedimentary layers.
Uses & applications
Historically used as a natural pigment (yellow ochre) for paints and dyes. Modern uses include clay manufacturing, land fill, and as a minor source of low-grade iron ore.
Geological facts
Rocks colored by limonite have been used as cave painting pigments since the Paleolithic period. The distinct yellow-orange color is often due to the oxidation of pyrite or other iron-bearing minerals localized in the sediment.
Field identification & locations
Identify by its earthy texture and mustard-yellow streak. It is commonly found in sedimentary basins and alongside weathered iron deposits. Collectors look for pieces with distinct layers or fossils.
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