The Yamuna
Explanation
The Himalayan drainage system consists of rivers that originate in the Himalayan mountain ranges, fed by melting glaciers and precipitation. The specific origin points of these rivers are distinct geographical features often located in the Greater Himalayas.
- The Yamuna: This river rises from the Yamunotri Glacier on the western slopes of the Banderpunch range (6,316 m) in the Uttarakhand Himalayas. It is the longest and the westernmost tributary of the Ganga.
- The Ganga: It originates as the Bhagirathi from the Gangotri Glacier near Gaumukh in the Uttarkashi district of Uttarakhand.
- The Ghaghara: This river originates from the Mapchachungo Glacier in the Tibetan Plateau near Lake Manasarovar.
- The Kosi: It is an antecedent river with its source to the north of Mount Everest in Tibet, where its main stream, the Arun, rises.
Key Takeaway: The Yamuna River originates specifically from the Yamunotri Glacier in the Banderpunch range, distinguishing it from other major Himalayan rivers like the Ganga and Ghaghara.