Rock Identifier
Septarian Nodule (Septarian Concretion) — sedimentary
sedimentary

Septarian Nodule

Septarian Concretion

AI-generated identification · may be incorrect

Hardness of 3.5 to 4 on the Mohs scale. Composed of calcite, aragornite, and limestone with brown, yellow, and grey colors and a dull to earthy luster.

Identified More sedimentary →
Explore Septarian Nodule in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness of 3.5 to 4 on the Mohs scale. Composed of calcite, aragornite, and limestone with brown, yellow, and grey colors and a dull to earthy luster.

Formation & geological history

Formed in sedimentary mudstone layers during the Cretaceous period approximately 50 to 100 million years ago through the dehydration and cracking of mud concretions.

Uses & applications

Popular as a decorative stone, polished display specimen, carved into spheres or bookends, and collected by mineral enthusiasts.

Geological facts

The distinctive crack patterns form when mud balls dry out and shrink from the inside out, creating cavities that later fill with minerals like calcite.

Field identification & locations

Easily identified by its characteristic turtle-shell pattern of internal cracks filled with contrasting minerals. Found globally, notably in Madagascar and Utah, USA.