
sedimentary
Siltstone with Iron Staining
Siltstone
Hardness: 3-4 (Mohs); Color: Grayish-green to tan with orange/red iron oxide (limonite) staining; Luster: Dull, earthy; Structure: Clastic, fine-grained; Cleavage: None (conchoidal or irregular fracture); Specific Gravity: 2.1-2.6
- Hardness
- 3-4 (Mohs)
- Luster
- Dull, earthy
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Physical properties
Hardness: 3-4 (Mohs); Color: Grayish-green to tan with orange/red iron oxide (limonite) staining; Luster: Dull, earthy; Structure: Clastic, fine-grained; Cleavage: None (conchoidal or irregular fracture); Specific Gravity: 2.1-2.6
Formation & geological history
Formed through the lithification of silt-sized particles in low-energy environments such as river floodplains, lagoons, or deep-water basins. Often Paleozoic to Cenozoic in age.
Uses & applications
Used primarily as low-grade construction fill, as a source for soil when weathered, or occasionally as a building stone if well-indurated.
Geological facts
Siltstone is differentiated from shale by its lack of fissility (it doesn't split into thin layers) and from sandstone by its smaller grain size, which feels smooth to the touch rather than gritty.
Field identification & locations
Identify in the field by its fine-grained texture that feels slightly gritty on the teeth but smooth to the fingers. Common in sedimentary basins worldwide. This specific specimen shows chemical weathering (oxidation).
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