Rock Identifier
Septarian Nodule (Calcite-filled Concretion) — sedimentary
sedimentary

Septarian Nodule

Calcite-filled Concretion

AI-generated identification · may be incorrect

Hardness 3.5 to 4 on Mohs scale, brownish exterior with yellow calcite veins, dull to vitreous luster, amorphous to microcrystalline structure.

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 3.5 to 4 on Mohs scale, brownish exterior with yellow calcite veins, dull to vitreous luster, amorphous to microcrystalline structure.

Formation & geological history

Formed in sedimentary mudstone layers during the Cretaceous period through the drying and cracking of iron-rich concretions filled with mineral-rich groundwater.

Uses & applications

Used primarily in lapidary arts, decorative carvings, metaphysical crystal collecting, and polished display pieces.

Geological facts

Septarian nodules often form around a fossil nucleus and are frequently called dragon stones due to their scaly, patterned appearance.

Field identification & locations

Identified by distinctive radial cracks filled with contrasting yellow calcite or aragonite. Commonly found in Madagascar, Utah, and England.