
sedimentary
Red Siltstone
Siltstone
Hardness: 3 to 4 on the Mohs scale. Color: Reddish brown due to iron oxide (hematite) staining. Luster: Dull or earthy. Crystal structure: Clastic/microcrystalline, composed mainly of quartz and clay minerals with grain sizes between 0.002 and 0.063 mm.…
- Hardness
- 3 to 4 on the Mohs scale
- Color
- Reddish brown due to iron oxide (hematite) staining
- Luster
- Dull or earthy
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Physical properties
Hardness: 3 to 4 on the Mohs scale. Color: Reddish brown due to iron oxide (hematite) staining. Luster: Dull or earthy. Crystal structure: Clastic/microcrystalline, composed mainly of quartz and clay minerals with grain sizes between 0.002 and 0.063 mm. Cleavage: Fissile along bedding planes if clay-rich, otherwise blocky. Specific gravity: 2.5 to 2.7.
Formation & geological history
Formed by the accumulation, compaction, and lithification of silt-sized mineral particles, typically in low-energy environments such as river floodplains, deltas, lakes, or deep-marine settings. Geological age ranges widely from Precambrian to recent.
Uses & applications
Used primarily in landscaping, crushed stone for construction, and occasionally as decorative building stone.
Geological facts
Red siltstone often preserves fine sedimentary structures like ripple marks and mud cracks, providing geologists with detailed clues about ancient environments.
Field identification & locations
Identified in the field by its fine-grained texture that feels slightly gritty between the teeth (distinguishing it from smoother shale), its distinct reddish-brown color, and lack of visible individual crystals without a microscope.
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