Mountains have usually formed on the edges of continents in narrow bands, where continents have collided in the past.
Crowders Mountain is part of the Appalachians, which formed during the Alleghenian Orogeny. The mountains formed when the continents of the time, Euramerica and Gondwana, collided to form the supercontinent Pangaea. The sections of the continents that collided correspond to the modern continents of Africa and North America.
The Ural Mountains were formed by the continents of Europe and Asia joining together.
The North American plate collided with the Pacific plate that created the rocky mountains.
The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.
The mountains in Pennsylvania were formed millions of years ago through tectonic plate movements and the collision of continents. The Appalachian Mountains, which run through Pennsylvania, were created when the North American Plate collided with the African Plate. Over time, erosion and glaciation further shaped the mountains into their current form.
Appalachian Mountains: Formed when the North American Plate collided with the African Plate. Himalayas: Created by the collision of the Indian Plate with the Eurasian Plate. Andes Mountains: Resulted from the subduction of the Nazca Plate beneath the South American Plate. Alps: Formed where the African Plate collided with the Eurasian Plate.
The Indian Plate and the Eurasian Plate collided to create the Himalaya mountains.
The Juan de Fuca Plate and the North American Plate
The Appalachians formed when North America and Africa collided. In time, the places separated and so much crust was created that the mountains were no longer at the plate boundary.
The Himalayan mountain range of Tibet was formed when the Indian Plate and the Eurasian Plate collided nearly 50 million years ago. It is the world's current mountain range and includes the world's tallest mountain, Mount Everest.
Africa and North America