
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 incorrectTypically 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.
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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.
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