The Appalachian Mountains of eastern North America are widely considered the oldest major mountain range on Earth. Their formation began over 480 million years ago (Ordovician Period) during the Taconic orogeny, followed by the Acadian, Alleghenian, and other collisions as ancestral continents (Laurentia, Gondwana, Avalonia) converged to form Pangaea.
Key facts:
Older individual rock formations exist (e.g., Canadian Shield, Greenland, Pilbara Craton >3.5 Ga), but as a continuous mountain system, the Appalachians are the senior range.