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Mountains can vary in height due to differences in tectonic processes such as plate collisions, volcanic activity, and erosion. Taller mountains are typically formed at convergent plate boundaries where two continental plates collide, pushing the Earth's crust upwards to create massive mountain ranges like the Himalayas. Erosion rates also play a role in determining mountain height, as faster erosion can wear down mountains quicker and result in lower peaks.

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1y ago

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