April 2024
Intermediate to advanced
592 pages
20h 6m
English
The collision between the Indian Plate and the Eurasian Plate, which started between 40 and 50 million years ago and is still going on now, is what gave rise to the Himalayan mountain range and Tibetan plateau. One plate could not subduct beneath the other due to the roughly same rock density of these two continental landmasses. The only way for the colliding plates to release their pressure was to shove upward, bend the collision zone, and create the jagged Himalayan peaks.
The world’s youngest mountain range is the Himalayas. The Tethys Sea is a massive geosyncline from which the Himalayan mountains emerged, and the uplift was divided into several stages. Pangaea, a supercontinent, ...
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