Rock Identifier
Polished septarian nodule slice (Septarian concretion, commonly calcite-filled cracks in a claystone/mudstone matrix (often with aragonite and brown iron oxides)) — sedimentary
sedimentary

Polished septarian nodule slice

Septarian concretion, commonly calcite-filled cracks in a claystone/mudstone matrix (often with aragonite and brown iron oxides)

AI-generated identification · may be incorrect

Typically brown, tan, and gray with polygonal dark crack patterns and a waxy-to-glassy polished luster; hardness about 3–4 for calcite-rich areas, with earthy claystone matrix. Septaria are irregular concretions, not true crystals, and may show calcite cleavage.

Identified More sedimentary
Explore Polished septarian nodule slice in the encyclopedia →

Identify your own rocks.

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

Physical properties

Typically brown, tan, and gray with polygonal dark crack patterns and a waxy-to-glassy polished luster; hardness about 3–4 for calcite-rich areas, with earthy claystone matrix. Septaria are irregular concretions, not true crystals, and may show calcite cleavage.

Formation & geological history

Forms when mud-rich sediment dries and contracts around a fossil or organic nucleus, producing cracks later filled by calcite or aragonite; many attractive specimens formed during the Cretaceous–Tertiary, roughly 65–50 million years ago.

Uses & applications

Used as decorative stones, cabochons, display specimens, and metaphysical curiosities; softer than most jewelry stones and susceptible to scratching.

Geological facts

The name derives from Latin septum, meaning “partition,” referring to the internal crack network. Polishing exposes the contrasting mineral-filled fractures and concentric concretion layers.

Field identification & locations

Identify it by its flattened nodule shape, brown clay-rich exterior, polygonal internal cracks, and cream or amber vein fillings; common sources include Utah and Madagascar. Avoid acids and prolonged soaking, which can etch calcite.