
sedimentary
Shale
Argillaceous Rock
AI-generated identification · may be incorrectMohs hardness: 2-3 (soft), Color: dark gray to brown, Luster: dull/earthy, Structure: laminated/fissile clastic, Cleavage: perfect parallel to bedding planes
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Physical properties
Mohs hardness: 2-3 (soft), Color: dark gray to brown, Luster: dull/earthy, Structure: laminated/fissile clastic, Cleavage: perfect parallel to bedding planes
Formation & geological history
Formed from the compaction of silt and clay-sized mineral particles, commonly in low-energy environments like lake beds or deep ocean basins. Ages range from the Archean to the Holocene.
Uses & applications
Used in the manufacture of cement, brick, tile, and as a filler in paint. It is also a primary source rock for oil and natural gas (shale gas).
Geological facts
Shale is the most common sedimentary rock on Earth, accounting for roughly 70 percent of the rocks in the crust. It often contains well-preserved fossils because of its fine grain size.
Field identification & locations
Identify in the field by its ability to split into thin sheets (fissility). It will often have a smooth feel but will not scratch glass. It is commonly found in river deltas and floodplains.
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