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During the Silurian Period, which lasted from approximately 443 to 419 million years ago, North Carolina was situated near the equator, in the southern part of the ancient supercontinent Gondwana. The region was primarily covered by shallow seas, leading to the deposition of marine sediments. The geological features from this period in North Carolina include limestone and other sedimentary rocks formed from the remains of marine life. Over millions of years, tectonic activity and erosion have significantly altered its position and landscape.

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6d ago

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