sedimentary

Shale

Fissile mudstone (primarily clay minerals and silt-sized quartz)

AI-generated identification · may be incorrect

Hardness: 3 on Mohs scale; Color: typically gray, brown, or black; Luster: dull/earthy; Crystal structure: lacks visible crystals; cleavage: fissile (splits into thin layers); Specific gravity: 2.4-2.8

Hardness: 3 on Mohs scale
Color: typically gray, brown, or black
Luster: dull/earthy

Identified May 12, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the compaction and lithification of silt and clay-sized mineral particles (mud) in slow-moving water environments like lagoons, floodplains, and deep ocean basins.

Uses & applications

Used in the production of cement, bricks, and tile. Fine-grained organic-rich shales are major sources of natural gas and petroleum (shale gas).

Geological facts

Shale is the most common sedimentary rock on Earth, making up an estimated 70 percent of the earth's crustal rocks. It often contains well-preserved fossils due to the fine grain size.

Field identification & locations

Identify in the field by its distinct layering and tendency to flake apart into thin, flat plates when struck. It is found globally in sedimentary basins.