
sedimentary
Argillite
Argillite (Fine-grained sedimentary rock composed mostly of clay-sized particles)
Hardness: 3-4 on the Mohs scale. Color: Brownish-red to dark brown. Luster: Dull or earthy. Crystal structure: Microcrystalline, amorphous clay minerals. Cleavage: Poor or none, breaks with a splintery or conchoidal fracture. Specific gravity: 2.5-2.7.
- Hardness
- 3-4 on the Mohs scale
- Color
- Brownish-red to dark brown
- Luster
- Dull or earthy
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Physical properties
Hardness: 3-4 on the Mohs scale. Color: Brownish-red to dark brown. Luster: Dull or earthy. Crystal structure: Microcrystalline, amorphous clay minerals. Cleavage: Poor or none, breaks with a splintery or conchoidal fracture. Specific gravity: 2.5-2.7.
Formation & geological history
Formed by the compaction and lithification of argillaceous sediments, mainly mud, silt, and clay. Typically deposited in quiet marine, lacustrine, or deltaic environments over millions of years.
Uses & applications
Used in educational geology collections, sometimes carved into ornamental objects or native art (such as Haida argillite carvings), and as a raw material in ceramics.
Geological facts
Argillite is intermediate in terms of metamorphism between shale and slate; it lacks the pronounced slaty cleavage of true slate.
Field identification & locations
Can be identified in the field by its fine-grained texture, earthy appearance, lack of fissility typical of shale, and dull luster. Common worldwide in sedimentary basins.
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