Rock Identifier
Septarian Nodule (Septarian Concretion (Calcite, Aragonite, Limestone, and Barite)) — sedimentary
sedimentary

Septarian Nodule

Septarian Concretion (Calcite, Aragonite, Limestone, and Barite)

AI-generated identification · may be incorrect

Hardness varies from 3 to 4 on the Mohs scale. Colors include brown, yellow, and grey, featuring a dull to vitreous luster and distinct calcified fracture patterns.

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Physical properties

Hardness varies from 3 to 4 on the Mohs scale. Colors include brown, yellow, and grey, featuring a dull to vitreous luster and distinct calcified fracture patterns.

Formation & geological history

Formed in sedimentary mudstone layers during the Cretaceous period, roughly 50 to 100 million years ago, through the shrinkage and mineral infilling of mud balls.

Uses & applications

Used primarily in lapidary arts, decorative carvings, home decor, and as a popular specimen for mineral collectors.

Geological facts

The distinctive spider-web pattern is created by shrinkage cracks that later fill with minerals like yellow calcite.

Field identification & locations

Easily identified by its turtle-shell-like pattern of radial cracks filled with contrasting minerals; commonly found in marine sedimentary deposits worldwide.