Rock Identifier
Siltstone / Fine-grained Graywacke (Argillaceous siltstone) — sedimentary
sedimentary

Siltstone / Fine-grained Graywacke

Argillaceous siltstone

Hardness: 3-5 (Mohs scale), Color: Dull gray to greenish-gray, Luster: Dull/Earthy with tiny sparkling mica specks, Texture: Fine-grained to clastic, Cleavage: Poorly developed (not fissile)

Identified More sedimentary

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Physical properties

Hardness: 3-5 (Mohs scale), Color: Dull gray to greenish-gray, Luster: Dull/Earthy with tiny sparkling mica specks, Texture: Fine-grained to clastic, Cleavage: Poorly developed (not fissile)

Formation & geological history

Formed from the accumulation and lithification of silt-sized particles (larger than clay, smaller than sand) in low-to-medium energy environments like river floodplains or marine basins.

Uses & applications

Commonly used as fill material, landscaping stone, or in the manufacturing of cement if the chemical composition is suitable. Small tumbled pieces are common beach or river pebbles.

Geological facts

Siltstones are midway between sandstones and shales. The tiny sparkling specks visible in the photo are likely small flakes of muscovite mica that reflect light.

Field identification & locations

Identified by its gritty feel on the teeth (grittier than clay/slate), fine-grained texture, and lack of distinct layering compared to shale. Found globally in sedimentary basins.