
sedimentary
Shale
Lutaceous sedimentary rock
Hardness: 3 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull or earthy; Crystal structure: Non-crystalline/fine-grained; Cleavage: Fissile (readily splits into thin layers); Specific gravity: 2.2 - 2.8
- Hardness
- 3 (Mohs scale)
- Color
- Dark grey to charcoal black
- Luster
- Dull or earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: Dark grey to charcoal black; Luster: Dull or earthy; Crystal structure: Non-crystalline/fine-grained; Cleavage: Fissile (readily splits into thin layers); Specific gravity: 2.2 - 2.8
Formation & geological history
Formed from the compaction and lithification of silt and clay-sized mineral particles (mud). It originates in low-energy environments such as river deltas, lake bottoms, and deep ocean basins over millions of years.
Uses & applications
Used primarily in the production of cement, bricks, and tiles. It is also a significant source rock for natural gas and petroleum through hydraulic fracturing.
Geological facts
Shale is the most common sedimentary rock on Earth, making up approximately 70% of the sedimentary rock in the Earth's crust. It often preserves fossils because of the fine-grained nature of the sediment.
Field identification & locations
Identify in the field by its distinct layering and dull appearance; it will often break into flat plates or thin chips when struck. Common in Appalachian mountains and river basins. Collectors should look for fossil imprints (ferns, shells) between layers.
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