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Koshi River

Koshi
Saptakoshi (सप्तकोसी)
River
Bhote Kosi in Nepal.jpg
Bhote Koshi in Nepal during the dry season. It is one of the tributaries of Koshi river.
Countries China, Nepal, India
States Shigatse Prefecture, Janakpur, Sagarmatha, Koshi, Mechi Zones, Bihar
Regions Tibet Autonomous Region, Eastern Development Region, Nepal, North-Central India
Cities Supaul (Bhaptiyahi), Purnia, Katihar
Source Sun Kosi, Arun and Tamur form Saptakoshi
 - location Tribenighat, Nepal
 - coordinates 26°54′47″N 87°09′25″E / 26.91306°N 87.15694°E / 26.91306; 87.15694
Mouth Ganges
 - location near Kursela, Bihar, India
 - coordinates 25°24′43″N 87°15′32″E / 25.41194°N 87.25889°E / 25.41194; 87.25889Coordinates: 25°24′43″N 87°15′32″E / 25.41194°N 87.25889°E / 25.41194; 87.25889
Length 720 km (447 mi)
Basin 74,500 km2 (28,765 sq mi)
Discharge
 - average 2,166 m3/s (76,492 cu ft/s)
River Ganges and tributaries.png
Map of the River Ganges and tributaries
Koshi River is located in India
Koshi River
Location of the mouth in India

The Koshi or Kosi River (Nepali: कोशी नदी, koshī nadī कोसी नदी, kosī nadī) drains the northern slopes of the Himalayas in the Tibet Autonomous Region and the southern slopes in Nepal. From a major confluence of tributaries north of the Chatra Gorge onwards, the Koshi River is also known as Saptakoshi (Nepali: सप्तकोशी, saptakoshī) for its seven upper tributaries. These include the Tamur Koshi originating from the Kanchenjunga area in the east, Arun River and Sun Koshi from Tibet. The Sun Koshi's tributaries from east to west are Dudh Koshi, Bhote Koshi, Tamba Koshi and Indravati Koshi. The Saptakoshi crosses into northern Bihar where it branches into distributaries before joining the Ganges near Kursela in Katihar district.

The Koshi is 720 km (450 mi) long and drains an area of about 74,500 km2 (28,800 sq mi) in Tibet, Nepal and Bihar. In the past, several authors proposed that the river has shifted its course for more than 133 km (83 mi) from east to west during the last 200 years. But a review of 28 historical maps dating 1760 to 1960 revealed a slight eastward shift for a long duration, and that the shifting was random and oscillating in nature.


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