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A 1908 map showing the course of the Ganges and its tributaries. Major left-bank tributaries include the Gomti River, Ghaghara River, Gandaki River and Kosi River; major right-bank tributaries include the Yamuna River, Son River, Punpun and Damodar. The hydrology of the Ganges River is very complicated, especially in the Ganges Delta region.
The Ganges Basin is a major part of the Ganges-Brahmaputra-Meghna (GBM) basin draining 1,999,000 square kilometres in Tibet, Nepal, India and Bangladesh. To the north, the Himalaya or lower parallel ranges beyond form the Ganges-Brahmaputra divide. On the west the Ganges Basin borders the Indus basin and then the Aravalli ridge.
It is the world's largest river delta [2] [3] and it empties into the Bay of Bengal with the combined waters of several river systems, mainly those of the Brahmaputra River and the Ganges River. It is also one of the most fertile regions in the world, thus earning the nickname the Green Delta.
The Ganges-Brahmaputra Delta is the river delta formed by the Ganges and Brahmaputra rivers when they enter the Bay of Bengal. Spread over the Bengal region, consisting of Bangladesh and the Indian state of West Bengal, it is the world's largest river delta and is one of the most fertile regions of the plains.
The Ganges river abruptly changed course 2,500 years ago following a devastating earthquake, according to a new study that raises concerns about the prevailing risk of megaquakes in South Asia.
As per the classification of Food and Agriculture Organization, the rivers systems are combined into 20 river units, which includes 14 major rivers systems and 99 smaller river basins grouped into six river units. The Ganges-Brahmaputra-Meghna basin is the largest, which covers 34% of the land area and contributes to nearly 59% of the available ...
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The Ganges Delta is “a really exciting place to work because it has these big, dynamic river channels,” said Dr. Elizabeth Chamberlain, lead author of a new study published June 17 in the ...