Rock Identifier
Red Claystone / Mudstone (Argillaceous sedimentary rock) — sedimentary
sedimentary

Red Claystone / Mudstone

Argillaceous sedimentary rock

Hardness: 2-3 (Mohs scale), Color: Reddish-brown to terracotta, Luster: Dull/Earthy, Crystal structure: Amorphous/Microcrystalline, Cleavage: None (conchoidal or irregular fracture), Texture: Fine-grained and crumbly.

Identified More sedimentary
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Physical properties

Hardness: 2-3 (Mohs scale), Color: Reddish-brown to terracotta, Luster: Dull/Earthy, Crystal structure: Amorphous/Microcrystalline, Cleavage: None (conchoidal or irregular fracture), Texture: Fine-grained and crumbly.

Formation & geological history

Formed from the lithification of mud and clay particles. The red color indicates the presence of iron oxides (hematite), suggesting formation in an oxygen-rich environment such as a river floodplain or desert basin.

Uses & applications

Used in the manufacture of bricks, ceramics, and pottery. In pulverized form, it can be used as a pigment (ochre) or as a filler in various industrial products.

Geological facts

Red beds, or sequences of red sedimentary rocks, are often associated with the Permian and Triassic periods and provide evidence of past arid or semi-arid climates on Earth.

Field identification & locations

Identified by its fine grain size, earthy feel, and tendency to break into blocky fragments rather than thin sheets (distinguishing it from shale). It often softens when wet.