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The formation of Superior Limestone and Columbia Limestone represents a significant geological transition during the Late Mississippian to Early Pennsylvanian periods. The Superior Limestone was primarily deposited in a shallow marine environment, characterized by warm, clear waters that favored the accumulation of carbonate materials. In contrast, Columbia Limestone formed later under different conditions, influenced by changes in sea level and sediment supply, leading to a more varied depositional environment that included both marine and non-marine influences. This shift reflects broader tectonic and climatic changes occurring during this time in Earth's history.

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