Appalachian Mountain Range
The Appalachian Mountains were created by the collision of eastern North America and Africa over 300 million years ago. This collision caused the formation of the supercontinent Pangaea, which eventually broke apart leading to the separation of these landmasses.
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The mountain range that is being created by the collision between the Indian tectonic plate and Asian tectonic plate is the Himalaya.
The Himalayas mountain range is formed by the collision of the Indian Plate with the Eurasian Plate. This collision has created some of the tallest peaks in the world, including Mount Everest.
The Appalachian region was created millions of years ago through geologic processes like plate tectonics and mountain-building events. The collision of tectonic plates pushed up the landmass, forming the Appalachian Mountains that span across eastern North America. Erosion and weathering over time have shaped the region into the diverse landscape we see today.
The Himalayan Mountain range was created by the collision of the Indian and Eurasian tectonic plates. This collision resulted in the uplift of the Earth's crust, forming the highest mountain range in the world. The ongoing movement of these plates continues to contribute to the growth of the Himalayas.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
Both plates collide and lift upward, forming moutains or mountain ranges.
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