
sedimentary
Shale or Slaty Mudstone
Argillaceous sedimentary rock
Hardness: 3-4 (Mohs scale); Color: Dark grey to charcoal, often with greenish hues from moss/lichen; Luster: Dull or earthy; Structure: Planar layers (fissility), fine-grained texture; Specific gravity: Approx. 2.5-2.8.
- Hardness
- 3-4 (Mohs scale)
- Luster
- Dull or earthy
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Physical properties
Hardness: 3-4 (Mohs scale); Color: Dark grey to charcoal, often with greenish hues from moss/lichen; Luster: Dull or earthy; Structure: Planar layers (fissility), fine-grained texture; Specific gravity: Approx. 2.5-2.8.
Formation & geological history
Formed from the compaction of silt and clay-sized mineral particles (mud) over millions of years. This specimen appears consistent with Paleozoic or Mesozoic formations common in forested temperate regions like the Appalachian or European highlands.
Uses & applications
Used primarily in the manufacture of cement, brick, and tile. If high in organic content, it can be a source of natural gas or oil. Low-grade slabs are used in landscaping and rustic walkways.
Geological facts
Shale is the most common sedimentary rock on Earth, making up about 70% of the sedimentary rock in the crust. Fossils are most likely to be preserved in this type of fine-grained sedimentary rock due to the low-oxygen environments in which it settles.
Field identification & locations
Identify by its ability to break along flat planes (fissility) and its soft, scratchable surface. It is often found in riverbeds or woodland outcrops. Collectors look for shale with fossil imprints or pyrite inclusions.
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