The Appalachian Mountains were formed primarily through a process known as continental collision during the Paleozoic Era, around 480 million years ago. This involved the collision of the North American and African tectonic plates, causing immense pressure and leading to the folding, faulting, and uplift of sedimentary rocks. Over millions of years, erosion has shaped the mountains, resulting in their current rounded peaks and valleys. The complex geological history includes multiple orogenies, notably the Alleghenian Orogeny, which played a significant role in their formation.
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