Septarian Nodules are concretions that have a series of radiating cracks, crossed by a series of concentric cracks to form a “turtle-back” appearance. Ball-like Sepatrian Nodules began their life as sedimentary slime at the bottom of a Cretaceous Sea 50 to 70 million years ago. Sediment composed of decomposing plants and animals formed into balls.
These Septarian Nodules are presented in a rare free-form display, suspended above a polished fossil round base.
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