Sun Koshi
सुनकोशी
The Koshi's central trunk — a world-class rafting river and the Sun Koshi–Marin diversion.
- River system
- Koshi
- Type
- Trans-Himalayan
- Length
- ≈257 km
- Basin area
- ≈3,394 km²
- Source
- The Bhote Koshi from the Tibet border in Sindhupalchok (the 'golden river')
- Outlet
- Gathers the Tama Koshi, Dudh Koshi and others, then joins the Arun and Tamor at Tribeni
- Provinces
- Bagmati, Koshi
The Sun Koshi's own upper catchment as given by Wikipedia, excluding the great tributaries (Tama Koshi, Dudh Koshi, Likhu) it gathers lower down.
The Sun Koshi ('golden river') is the trunk into which the Koshi system's western rivers drain. Its principal headstream, the Bhote Koshi, descends from Nyalam County in Tibet through the Arniko Highway corridor; at Dolalghat the Indrawati joins, and from there the river turns east along the foot of the Mahabharat range, absorbing the Tama Koshi, Likhu and Dudh Koshi one after another on its long run to Tribeni, where it meets the Arun and Tamor to form the Sapta Koshi.
It is a corridor that lives with Himalayan hazard. On 2 August 2014 a massive landslide at Jure in Sindhupalchok killed around 155 people, destroyed more than a hundred houses, and dammed the river outright — the impounded lake submerged the highway and the blockage cut power generation until the army blasted a channel through the debris.
The Sun Koshi's long, continuous whitewater is its other claim to fame: the classic multi-day rafting expedition runs about 272 km from Dolalghat (620 m) down to the Chatara gorge (115 m) on grade III–IV rapids, and is regularly ranked among the world's great river journeys.
The river also works hard. The Bhote Koshi corridor carries a string of hydropower plants, and in Sindhuli the river is the donor for the Sunkoshi–Marin Diversion, a National Pride Project since January 2020: a 13.3 km tunnel — bored by TBM and broken through on 8 May 2024, well ahead of schedule — will divert a design flow of 67 m³/s into the Marin Khola of the Bagmati basin, irrigating some 122,000 ha across five Madhesh districts and generating 38.62 MW on the way.
Course and geography
The Sun Koshi (also spelled Sunkoshi) is one of the principal rivers of central and eastern Nepal and the central trunk of the larger Koshi (Sapta Koshi) river system. Its name combines the Nepali words sun, meaning gold or golden, and koshi, meaning river, so it is widely known as the "golden river" — a reference to the shimmering, sediment-laden sand that gives its waters and banks a golden cast.
The river is fed from two source streams in the high Himalaya. The more significant headwater originates in the Zhangzangbo Glacier region of Nyalam County, in the Tibet Autonomous Region of China, at an elevation of around 5,300 metres, while a second source stream rises within Nepal near Choukati at roughly 2,400 metres. From the Tibetan border the river flows generally eastward, threading the long structural valley between the Mahabharat (Lesser Himalaya) range to the south and the High Himalaya to the north.
Descending steeply from the mountains, the Sun Koshi loses considerable elevation along its course — dropping from around 620 metres at Dolalghat to roughly 115 metres by the time it reaches the Chatra Gorge near the southern plains. Below the gorge the combined Koshi system spills onto the Terai and Gangetic plain. The river is best known to travellers for its long navigable reach of about 270–272 kilometres between Dolalghat and Chatara, near the Nepal-India border.
Hydrology and tributaries
The Sun Koshi gathers the drainage of a large swath of central Nepal, collecting waters from several major Himalayan tributaries as it flows east. Its right-bank tributaries include the Bhote Koshi (known as the Matsang/Poiqu in Tibet) and the Indrawati, while its principal left-bank tributaries are the Tama (Tamba) Koshi, the Likhu Khola and the Dudh Koshi, which itself drains the Everest region. Through these tributaries the Sun Koshi integrates snowmelt, glacial melt and monsoon runoff from a very large mountainous catchment.
Near the foothills the Sun Koshi meets the Arun and the Tamur rivers at Tribeni (Tribenighat). The union of these three rivers forms the Sapta Koshi — the "Seven Koshis" — which then cuts through the Chatra Gorge and flows south into the Indian state of Bihar before joining the Ganges. Of the water entering the Sapta Koshi, the Sun Koshi contributes the largest single share, on the order of 44 percent, compared with roughly 37 percent from the Arun and about 19 percent from the Tamur, underscoring its role as the central trunk of the system.
The river carries a heavy sediment load characteristic of young, fast-eroding Himalayan terrain. This high sediment yield is a defining feature of the wider Koshi system and contributes both to the river's golden appearance and to the chronic engineering and flood-management challenges faced downstream on the plains.
Economic significance: irrigation and hydropower
The Sun Koshi is increasingly important to Nepal's energy and irrigation ambitions. The Sun Koshi Hydropower Station, a run-of-river plant in Sindhupalchok District commissioned in 1972, has an installed capacity of about 10.05 MW supplied by three Francis turbines. Several much larger schemes have been studied or proposed along the river, including the planned Sunkoshi-3, a project envisaged at hundreds of megawatts of installed capacity, reflecting the river's substantial untapped hydropower potential.
The most prominent current development is the Sunkoshi-Marin Diversion Multipurpose Project, designated one of Nepal's National Pride Projects and overseen by the Ministry of Energy, Water Resources and Irrigation. It is an inter-basin transfer designed to divert water from the Sun Koshi into the Marin, a tributary of the Bagmati, augmenting the Bagmati Irrigation System. A major milestone came in early May 2024 when a Robbins double-shield tunnel boring machine completed the project's roughly 13.3-kilometre headrace tunnel, breaking through ahead of schedule despite difficult geology.
Once operational, the Sunkoshi-Marin scheme is intended to provide year-round irrigation to around 122,000 hectares of farmland across the southern districts of Rautahat, Bara, Sarlahi, Mahottari and Dhanusha, while also generating about 31 MW of electricity. Proposals such as the Sunkoshi-Kamala diversion — which would transfer water through a long tunnel to a powerhouse and on to the Kamala basin for irrigation and power — illustrate the river's strategic position in Nepal's plans to move Himalayan water to the dry, populous Terai.
Cultural importance and whitewater rafting
Within the wider Koshi system, the Sun Koshi holds a place of cultural and regional significance, its valley long serving as a historic corridor linking the Kathmandu region with the eastern hills and the Tibetan frontier. As the central feeder of the Sapta Koshi — a river deeply woven into the sacred geography and livelihoods of both Nepal and northern India — the Sun Koshi is part of one of the subcontinent's most storied river networks.
In modern times the river has gained international fame as a premier whitewater destination. The Sun Koshi rafting expedition, running roughly 270 kilometres from Dolalghat to Chatara near the Indian border, is the longest river journey in Nepal and is frequently ranked among the world's great multi-day river trips. Depending on water levels it offers rapids generally graded III to IV (with harder, grade-V conditions at high flows), with named features such as Harkapur, Dead Man's Eddy, Rhino Rock and Meat Grinder challenging experienced paddlers.
The classic descent typically takes about one to two weeks, passing through remote gorges, forested hills and riverside villages, with camping on the river's golden sandbars. The most reliable seasons are the post-monsoon months from roughly September to December and the spring window of March to May, when water levels and weather are most favourable. The first recorded full descent of the river was made in 1970.
Environment and hazards
Like much of the Himalaya, the Sun Koshi basin is prone to powerful and sometimes catastrophic natural hazards. Steep slopes, fragile geology, intense monsoon rainfall and seismic activity combine to produce frequent landslides, debris flows and glacial hazards, several of which have had severe consequences for communities and infrastructure along the river.
One of the most destructive recent events was the Jure landslide of 2 August 2014, when a massive rainfall-triggered rockslide in Sindhupalchok District buried Jure village, killing roughly 155 people and destroying scores of houses. The slide dammed the Sun Koshi, forming a natural barrier and a lake several kilometres long upstream and raising fears of a sudden dam-break flood; it also severed the Araniko Highway, the main road link toward the Chinese border. Authorities undertook controlled measures to lower the lake, and the landslide dam was eventually breached.
The river's high-altitude headwaters also expose it to glacial lake outburst floods (GLOFs). In 1981 an ice avalanche triggered an outburst from the moraine-dammed Zhangzangbo Cho in Tibet, sending a destructive flood down the upper river system and damaging bridges and highway sections. Such events, together with the basin's heavy sediment transport, mean that flood risk, slope stability and the safety of dams and diversion works remain central environmental concerns for the Sun Koshi and the downstream Koshi plains.
Key facts
| Name meaning | "Golden river" (Nepali sun = gold, koshi = river) |
| Headwaters | Zhangzangbo Glacier region, Nyalam County, Tibet (China); also a stream rising at Choukati, Nepal |
| Source elevation | Tibetan stream ~5,300 m; Nepali stream ~2,400 m |
| Major tributaries | Bhote Koshi, Indrawati, Tama (Tamba) Koshi, Likhu Khola, Dudh Koshi |
| Confluence | Joins Arun and Tamur at Tribeni to form the Sapta Koshi |
| Share of Sapta Koshi flow | ~44% (Arun ~37%, Tamur ~19%) |
| Rafting run | ~270-272 km, Dolalghat to Chatara; grade III-IV+ rapids; among the world's classic multi-day expeditions |
| Sunkoshi Hydropower Station | 10.05 MW run-of-river plant, Sindhupalchok, commissioned 1972 |
| Sunkoshi-Marin Diversion | National Pride Project; ~13.3 km tunnel (breakthrough May 2024); ~31 MW; irrigates ~122,000 ha |
| 2014 Jure landslide | 2 Aug 2014; ~155 deaths; dammed the river, forming an upstream lake |
Main tributaries
The Sun Koshi (highlighted) shown with the rest of the Koshi system. Real river courses from OpenStreetMap — hover to label, click to switch river.
Hydropower on the Sun Koshi
15 catalogued plants on or fed by this river, 2,694 MW in total. Tap any plant for its full profile.
| Plant | Capacity | Stage | District |
|---|---|---|---|
| Sunkoshi-2 Storage Hydroelectric Project | 1,110 MW | Proposed | Sindhuli / Ramechhap |
| Sunkoshi-3 Storage / Multipurpose Project | 683 MW | Proposed | Kavrepalanchok / Ramechhap |
| Upper Trishuli-1 Hydroelectric Project | 216 MW | Under construction | Rasuwa |
| Rasuwa Bhotekoshi Hydroelectric Project | 120 MW | Under construction | Rasuwa |
| Rasuwagadhi Hydroelectric Project | 111 MW | Operational | Rasuwa |
| Madhya Bhotekoshi Hydroelectric Project | 102 MW | Operational | Sindhupalchok |
| Super Trishuli Hydropower Project | 100 MW | Under construction | Nuwakot |
| Upper Trishuli 3A Hydropower Station | 60 MW | Operational | Nuwakot |
| Bhote Koshi Power Plant (Upper Bhotekoshi) | 45 MW | Operational | Sindhupalchok |
| Bhotekoshi-1 Hydroelectric Project | 40 MW | Under construction | Sindhupalchowk |
| Upper Trishuli-3B Hydroelectric Project | 37 MW | Under construction | Nuwakot |
| Trishuli Hydropower Station | 24 MW | Operational | Nuwakot |
| Upper Chaku A Hydropower Project | 22 MW | Operational | Sindhupalchok |
| Devighat Hydropower Station | 14 MW | Operational | Nuwakot |
| Sunkoshi Hydropower Station | 10 MW | Operational | Sindhupalchok |
More in the Koshi system
Koshi (Sapta Koshi)
Nepal's largest river system — the 'Sapta Koshi', seven rivers in one — and the 'Sorrow of Bihar' for its floods
Arun
An 'antecedent' river older than the Himalaya it cuts through — and home to the 900 MW Arun-3
Tama Koshi (Tamakoshi)
The river behind Upper Tamakoshi — Nepal's single largest hydropower plant at 456 MW
Dudh Koshi
Everest's own river — the 'milk river' fed by Khumbu glaciers, and a major storage-project candidate
Tamor
The easternmost of the seven Koshis, draining Kanchenjunga
Sun Koshi: frequently asked questions
How long is the Sun Koshi?+
The Sun Koshi is about 257 km long.
Where does the Sun Koshi start?+
The Sun Koshi rises at The Bhote Koshi from the Tibet border in Sindhupalchok (the 'golden river'). It empties at Gathers the Tama Koshi, Dudh Koshi and others, then joins the Arun and Tamor at Tribeni.
Which river system does the Sun Koshi belong to?+
The Sun Koshi is part of the Koshi river system. Rises on the Tibetan plateau and cuts through the Himalaya.
What are the main tributaries of the Sun Koshi?+
Its main tributaries include Bhote Koshi, Indrawati, Tama Koshi, Likhu, among others.
What hydropower is built on the Sun Koshi?+
15 catalogued hydropower plants are on or fed by the Sun Koshi, totalling 2,694 MW. The largest is Sunkoshi-2 Storage Hydroelectric Project at 1,110 MW in Sindhuli / Ramechhap.
Sources & data note
River length and drainage figures are approximate. The mapped course is the real river centreline from OpenStreetMap, clipped to Nepal. Hydropower figures are from our own source-cited hydro database.
- Sun KosiWikipedia ↗
- Sunkoshi Marin Diversion ProjectWikipedia ↗
- Kosi RiverWikipedia ↗
- Koshi Basin InitiativeICIMOD ↗
- River geometry — OpenStreetMap© OpenStreetMap contributors ↗
- Rivers of Nepal — overviewWikipedia ↗
- Department of Hydrology and MeteorologyGovernment of Nepal, DHM ↗
- Water and Energy Commission Secretariat (WECS)Government of Nepal, WECS ↗
- Sunkoshi RiverWikipedia ↗
- Sunkoshi-Marin Diversion tunnel breakthroughFiscal Nepal ↗
- 2014 Sunkoshi blockage (Jure landslide)Wikipedia ↗
- Sunkoshi Hydropower StationWikipedia ↗