Rock Identifier
Shale (Sedimentary rock composed of clay minerals and quartz) — sedimentary
sedimentary

Shale

Sedimentary rock composed of clay minerals and quartz

Hardness: 3 on Mohs scale; Color: Black/dark grey; Luster: Dull/earthy; Structure: Clastic, fine-grained, fissile (splits into thin layers)

Hardness
3 on Mohs scale
Color
Black/dark grey
Luster
Dull/earthy
Identified More sedimentary
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Physical properties

Hardness: 3 on Mohs scale; Color: Black/dark grey; Luster: Dull/earthy; Structure: Clastic, fine-grained, fissile (splits into thin layers)

Formation & geological history

Formed through the compaction and lithification of silt and clay-sized mineral particles, often in low-energy environments like lake bottoms or deep ocean basins.

Uses & applications

Used as a raw material for brick, tile, and pottery; some varieties are sources of oil and natural gas (shale gas).

Geological facts

Shale is the most common sedimentary rock on Earth. It often contains fossils of microorganisms and plants due to the gentle deposition process.

Field identification & locations

Identify by its thin, flat layers (fissility) and soft texture that can often be scratched with a fingernail or penny. Found globally in basins and river deltas.