
sedimentary
Earthy Siltstone with Iron Staining
Siltstone / Argillite with Goethite/Hematite inclusions
Hardness: 3-5 (variable); Color: Tan, brown, and grey with reddish-brown oxidation; Luster: Dull/Earthy; Crystal structure: Clastic (microscopic grain size); Cleavage: None (conchoidal to irregular fracture)
- Hardness
- 3-5 (variable)
- Color
- Tan, brown, and grey with reddish-brown oxidation
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3-5 (variable); Color: Tan, brown, and grey with reddish-brown oxidation; Luster: Dull/Earthy; Crystal structure: Clastic (microscopic grain size); Cleavage: None (conchoidal to irregular fracture)
Formation & geological history
Formed by the compaction and lithification of silt-sized particles often deposited in low-energy environments like river floodplains or lake beds. The reddish-brown layers indicate oxidation of iron minerals within the sedimentary layers.
Uses & applications
Commonly used as fill material in construction or as a source of aggregate. In some cases, siltstones with high clay content are used for making bricks or tiles.
Geological facts
Siltstone is intermediate between sandstone and shale. If the grains are too small to be seen but can be felt as 'gritty' against the teeth, it is classified as siltstone rather than claystone.
Field identification & locations
Identified in the field by its fine-grained texture that is grittier than shale but smoother than sandstone. It often displays thin laminations. Found in sedimentary basins worldwide.
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