
sedimentary
Siltstone
Siltstone (clastic sedimentary rock)
Hardness: 3-5 (Mohs scale); Color: Tan, beige, light brown; Luster: Dull, earthy; Crystal structure: Non-crystalline clastic; Cleavage: None/Planar (fissility); Specific gravity: 2.1-2.6
- Hardness
- 3-5 (Mohs scale)
- Color
- Tan, beige, light brown
- Luster
- Dull, earthy
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Physical properties
Hardness: 3-5 (Mohs scale); Color: Tan, beige, light brown; Luster: Dull, earthy; Crystal structure: Non-crystalline clastic; Cleavage: None/Planar (fissility); Specific gravity: 2.1-2.6
Formation & geological history
Formed from the lithification of silt-sized particles deposited in low-energy environments such as river floodplains, lake beds, or marine shelves. These particles are smaller than sand but larger than clay.
Uses & applications
Used primarily in construction as fill material or road base. Occasionally used for exterior landscaping or as a budget-friendly flagstone when well-cemented.
Geological facts
Siltstone differs from shale by its lack of fissility (thin layer splitting) and from sandstone by its significantly smoother texture to the touch.
Field identification & locations
Identify in the field by its fine-grained texture that feels slightly gritty against the teeth but smooth to the fingers. Common in sedimentary basins worldwide.
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Arenite (if sandstone)
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Brecciated Chert (Microcrystalline Silica)
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Sandstone
Arenite (primarily SiO2)
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