Rock Identifier
Septarian Nodule (Septarian Concretion) — sedimentary
sedimentary

Septarian Nodule

Septarian Concretion

AI-generated identification · may be incorrect

Hardness 3.5 to 4 on the Mohs scale, featuring a distinctive mosaic of brown calcite, grey limestone, and yellow barite. Luster is dull to vitreous with a massive crystal structure.

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Physical properties

Hardness 3.5 to 4 on the Mohs scale, featuring a distinctive mosaic of brown calcite, grey limestone, and yellow barite. Luster is dull to vitreous with a massive crystal structure.

Formation & geological history

Formed during the Cretaceous period roughly 50 to 100 million years ago when mud-rich sediments accumulated and cracked as they dried or shrank, allowing mineral-rich waters to precipitate veins inside.

Uses & applications

Popular in ornamental carvings, lapidary arts, and as highly prized decorative display specimens for mineral collectors.

Geological facts

Septarian nodules are often called dragon stones due to their reptilian pattern of intersecting mineral veins.

Field identification & locations

Easily identified by the prominent network of radial cracks filled with contrasting minerals; commonly found in sedimentary clay deposits, notably in Madagascar and Utah.