Mount Mansfield Live Cam

The Geological Origins

Mount Mansfield, the highest peak in Vermont, is a prominent feature of the Green Mountains, boasting a striking natural history that dates back millions of years. The mountain was formed during the Taconic orogeny, a major geological event that reshaped the region during the late Ordovician period. The bedrock of Mount Mansfield is primarily composed of schist and phyllite, indicative of intense pressure and heat that transformed sedimentary rocks into metamorphic formations. These ancient rocks tell the story of continental collisions and the dynamic processes that shaped the northeastern United States.