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Raccoon Mountain is found in a band of limestone from the Mont eagle Arrangement, which shaped amid the Mississippian Period (around 320-360 million a long time prior), on the foot of an old ocean. In this ocean, parts and shells of different marine creatures sank to the foot and got to be compacted over time to make limestone shake. Raccoon Mountain has fossils of crinoids, coral, bryozoans, and echinoderms throughout their cave. In spite of the fact that fossils within the limestone tell them the age of the shake, they are not much offer assistance in deciding the age of the cave. Most caves, counting their own, are less than ten million a long time old. By the conclusion of the Permian Period (approximately 225 million a long time prior), colossal mountain building strengths coming about from the collision of the landmasses constrained the oceans to withdraw.