
sedimentary
Siltstone
Siltstone
Hardness: 3-4 (Mohs); Color: Grey, brown, or reddish-brown; Luster: Dull/Earthy; Crystal structure: Non-crystalline clastic; Cleavage: None, can show fissility; Specific gravity: 2.3-2.6
- Hardness
- 3-4 (Mohs)
- Color
- Grey, brown, or reddish-brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3-4 (Mohs); Color: Grey, brown, or reddish-brown; Luster: Dull/Earthy; Crystal structure: Non-crystalline clastic; Cleavage: None, can show fissility; Specific gravity: 2.3-2.6
Formation & geological history
Formed through the lithification of silt-sized particles deposited in slow-moving water environments like floodplains, deltas, or lakes. Most specimens range from Paleozoic to Cenozoic eras.
Uses & applications
Used primarily as low-quality fill material in construction, as a source of soil minerals, and occasionally for decorative landscaping or flagstones if sufficiently durable.
Geological facts
Siltstone is intermediate between sandstone and shale; it has smaller grains than sandstone but lacks the extreme clay content and thin layering of true shale.
Field identification & locations
Identify by its gritty feel on teeth (unlike shale) but smooth appearance compared to sandstone. Commonly found in sedimentary basins and river outcrops.
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