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A look at the geologic history of Mount Everest, the tallest peak in the world, and how the Himalayas mountain range was really once an ancient seabed, pushed up to the roof of the world by tectonic smashing of the Indian plate into the Asian continent. The convergence of processes that resulted in the extreme height of Mt. Everest and the other Himalayan mountains is explained in conjunction with the supporting geological evidence. (2010) History Channel