Around 200 million years ago, the Himalayan mountains were not yet in their current form. At that time, they were part of the ancient supercontinent Pangaea, characterized by flat, low-lying land and oceanic environments. The collision of the Indian and Eurasian tectonic plates, which began around 50 million years ago, eventually led to the uplift of the Himalayas, transforming the landscape into the towering peaks we see today.
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