The document summarizes how the Himalayas and Tibetan Plateau formed through the collision of the Indian and Eurasian tectonic plates starting around 130 million years ago. Sediment deposited on the ocean floor was subducted or squeezed up to form the highest mountains, as evidenced by fossils like ammonites found high in the mountains. The Indian plate drifted northward into Asia, and the continental crust behaved plastically when compressed under pressure, folding and uplifting to create the Himalayan range.