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The Appalachian Mountains were formed primarily through tectonic processes over hundreds of millions of years. Their origins date back to the Paleozoic Era, around 480 million years ago, when continental collisions and volcanic activity caused the land to buckle and fold. This mountain-building event, known as the Appalachian Orogeny, was further shaped by erosion and sedimentation over time, resulting in the rugged terrain we see today. The mountains continue to evolve due to ongoing geological processes.

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