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The Krishna River has 13 major tributaries. [10] Its principal tributaries include the Ghataprabha River, Malaprabha River, Bhima River, Tungabhadra River and Musi River. [10] The Tungabhadra River has a catchment area of 71,417 km 2 (27,574 sq mi) and a length of 531 km (330 mi). [10] The Bhima River is the longest tributary of the Krishna ...
Pearl River - China - South China Sea; Penna River-India; Periyar River-India-Kerala; Rajang River - Malaysia - South China Sea; Ravi River - Pakistan and India; Red River - China, Vietnam - South China Sea; Rio Grande de Mindanao - Philippines; Sabarmati River-India; Sakarya River - Turkey; Salween - China (Tibet, Yunnan), Myanmar, Thailand ...
This is a list of longest rivers of Asia. Included are all rivers with lengths over 1,000 km (620 mi) that are in Asia. ... China: 6,300 3,915 2 Yellow River ...
Most of the rivers in India originate from the four major watersheds in India. The Himalayan watershed is the source of majority of the major river systems in India including the three longest rivers–the Ganges, the Brahmaputra and the Indus. [3] [4] These three river systems are fed by more than 5000 glaciers. [5]
"China River Basins". WorldMap. Harvard University. Interactive map with China's river basins, showing river names in Chinese. Table of rivers in China with Chinese names and useful data (dead link 01:15, 4 March 2013 (UTC))
A History of East Asia: From the Origins of Civilization to the Twenty-First Century (2010). Huffman, James L. Japan in World History (Oxford, 2010) Jansen, Marius B. Japan and China: From War to Peace, 1894-1972 (1975) Karl, Rebecca E. "Creating Asia: China in the world at the beginning of the twentieth century."
These varying definitions are not generally reflected in the map of Asia as a whole; for example, Egypt is typically included in the Middle East, but not in Asia, even though the bulk of the Middle East is in Asia. The demarcation between Asia and Africa is the Suez Canal, the Gulf of Suez, the Red Sea, and the Bab-el-Mandeb.
The Brahmaputra River experiences two high-water seasons, one in early summer caused by snowmelt in the mountains, and one in late summer caused by runoff from monsoon rains. The river flow is strongly influenced by snow and ice melting of the glaciers, which are located mainly on the eastern Himalaya regions in the upstream parts of the basin.