During this collision, the edges of the colliding tectonic plates were subjected to immense pressure and heat, causing the Earth's crust to fold, buckle, and uplift. The resulting geological forces were responsible for the formation of Cadillac Mountain and the surrounding peaks of Mount Desert Island.
Over time, the subsequent cooling and erosion of the Earth's surface have further shaped Cadillac Mountain into the iconic feature we know today. Glaciers during various ice ages played a crucial role in sculpting the landscape, creating the U-shaped valleys and rugged cliffs that characterize Acadia National Park.
Therefore, the formation of Cadillac Mountain can be traced back to the tectonic forces of the Acadian orogeny and the subsequent molding effects of glaciers, making it a fascinating geological marvel within the context of the Appalachian Mountain range.
