sedimentary
Ironstone Concretion / Limonite-stained Siltstone
Ironstone (primarily Limonite FeO(OH)·nH2O and Siltstone)
Hardness: 4-5.5 (variable); Color: Ochre, rusty orange, dark brown; Luster: Dull, earthy; Crystal structure: Amorphous to microcrystalline; Cleavage: None (conchoidal or irregular fracture); Specific Gravity: 2.7–4.3 depending on iron content.
- Hardness
- 4-5
- Color
- Ochre, rusty orange, dark brown
- Luster
- Dull, earthy
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Physical properties
Hardness: 4-5.5 (variable); Color: Ochre, rusty orange, dark brown; Luster: Dull, earthy; Crystal structure: Amorphous to microcrystalline; Cleavage: None (conchoidal or irregular fracture); Specific Gravity: 2.7–4.3 depending on iron content.
Formation & geological history
Formed by the precipitation of iron-rich minerals (limonite, goethite, or hematite) within the pore spaces of sedimentary layers, often silt or clay. These minerals act as a cement, binding the sediment into a hard, weather-resistant mass. Often found in Phanerozoic sedimentary basins.
Uses & applications
Ochre versions are used as natural pigments. Generally used as low-grade iron ore or crushed stone for road fill. Significant mainly for educational geological collections and hobbyist 'rock hounding' due to unique shapes.
Geological facts
These are often mistaken for fossils or meteorites because of their unusual shapes and high density. In some regions, they are known as 'shale balls' or 'iron balls.' The heart-like shape of this specimen is a result of natural weathering and differential erosion.
Field identification & locations
Identify by its distinctive rusty orange color (iron oxidation) and its weight, which is often heavier than surrounding sandstone or shale. Found frequently in riverbeds or coastal cliffs where sedimentary layers are exposed.
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