AmarnepalNepal Data
Southern / Mahabharat system · Mahabharat

Bagmati

बागमती

Kathmandu's holy river, flowing past the Pashupatinath temple.

River system
Southern / Mahabharat
Type
Mahabharat
Length
≈195 km
Source
The Bagdwar springs in the Shivapuri hills, north of Kathmandu
Outlet
Crosses into India and joins the Koshi/Ganga in Bihar
Provinces
Bagmati, Madhesh

≈195 km in Nepal; ≈586 km in total to its outfall in Bihar (Wikipedia).

The Bagmati rises at Bagdwar — the 'tiger's mouth' spring at about 2,740 m in the Shivapuri hills of what is now Shivapuri Nagarjun National Park — and flows down through the Kathmandu Valley, separating the old royal cities of Kathmandu and Patan and gathering the Bishnumati, Manohara and Nakkhu along the way. It then cuts south through the Mahabharat range to the Madhesh plains and on into Bihar, where its waters eventually reach the Koshi.

No Nepali river carries more religious weight per cubic metre. At Pashupatinath — the great temple of Shiva on its banks, part of the Kathmandu Valley UNESCO World Heritage Site inscribed in 1979 — Hindus are cremated at the riverside ghats, the dead traditionally dipped three times in the Bagmati before the pyre is lit. For the valley's civilisation, Newar and Hindu alike, the Bagmati is the axis of ritual life from birth to death.

That sanctity collides with the valley's sewage. Through Kathmandu the river receives large volumes of untreated waste — the Bishnumati tributary is the most degraded — and restoring it has become a civic cause: the Bagmati Mega Clean-Up Campaign, launched in 2013, has mobilised volunteers, officials and soldiers every Saturday for years, alongside donor-funded basin-improvement works.

Hydrologically the Bagmati is a Mahabharat-origin river — fed by springs and monsoon rain rather than glaciers, so its flow swings sharply between seasons. Its Kulekhani tributary, impounded by a 114 m dam to form the Indra Sarovar reservoir, feeds the Kulekhani I, II and III stations (60 + 32 + 14 = 106 MW) — Nepal's only seasonal-storage hydropower, the battery the grid leans on in the dry months. Downstream, the Bagmati Irrigation System waters the central Tarai, soon to be augmented by Sun Koshi water via the Sunkoshi–Marin tunnel.

In depth

Course and geography

The Bagmati River rises in the Shivapuri hills on the northern rim of the Kathmandu Valley, conventionally traced to the Baghdwar ("Tiger Gate") spring near Sundarijal, inside the Shivapuri Nagarjun National Park, at an elevation of roughly 2,740 metres (about 8,990 feet). At Baghdwar the source water issues from a stone spout carved in the shape of a tiger's mouth, a feature that gives the spot both its name and its long-standing sacred associations.

From its headwaters the river flows generally southwest across the floor of the Kathmandu Valley, where it has historically separated the twin cities of Kathmandu and Patan (Lalitpur). After threading the valley and passing the Pashupatinath temple complex, the Bagmati cuts through the surrounding hills and descends onto the plains of Nepal's Madhesh Province before crossing the international border into the Indian state of Bihar.

The river is reported to have a total length of about 586 kilometres (roughly 364 miles) from its Himalayan source to its end on the Gangetic plain. In Bihar it eventually meets the Kamala River, and its waters ultimately reach the larger Ganges (Ganga) river system. The Bagmati is unusual among major Nepali rivers in that it is fed by rainfall and groundwater rather than by Himalayan glacial melt, which makes its flow highly seasonal and strongly tied to the summer monsoon.

Hydrology and tributaries

As a monsoon-fed, non-glacial river, the Bagmati's discharge varies dramatically between the dry winter and the wet summer. Flows can shrink to a thin, polluted trickle through Kathmandu in the dry season and then surge enormously during heavy monsoon rains, a regime that drives both its water-scarcity problems in the valley and its flood hazard downstream.

Within and around the Kathmandu Valley the river gathers numerous tributaries. The Bishnumati, which drains the western side of the valley, is among its most important right-bank tributaries, while the Manohara joins from the east near the Pashupatinath area. Smaller valley streams such as the Dhobi Khola (Rudramati) and the Tukucha (Tukucha Khola) also feed into it; several of these urban streams carry large volumes of untreated sewage into the main river.

Below the valley the Bagmati continues to collect tributaries on the plains, including the Marin Khola, Lakhandei, Adhwara and Lalbakaiya. In its lower reaches the river can carry very large flood discharges, illustrating the scale of the flows the river can produce after intense rainfall on its monsoon-dominated catchment.

Economic significance

The Bagmati's greatest economic role lies on the Terai plains, where it supports large-scale irrigation. The Bagmati Irrigation Project, drawing water from the river via the Bagmati Barrage near Karmaiya, is designed to irrigate a substantial command area across Sarlahi and Rautahat districts, supporting paddy and other crops in Nepal's central Terai agricultural belt.

The river basin has also long been studied for hydropower potential. Plans associated with the Bagmati barrage and broader basin development have envisioned a higher dam and electricity generation alongside expanded irrigation, though such schemes have faced lengthy delays and only partial implementation over several decades. The Bagmati River Basin Improvement Project and related government and donor-supported programmes have aimed to modernise infrastructure and improve integrated water management across the basin.

Within the Kathmandu Valley the river's economic value is more closely tied to water supply, religious tourism and the surrounding heritage economy than to large engineering works. Reservoir and recharge schemes such as the Dhap Dam in the upper catchment have been promoted to augment dry-season flow and help restore the river through the city. Figures for irrigated area, project costs and proposed generating capacity have varied over time and across sources, and should be treated as approximate.

Cultural and religious importance

The Bagmati is one of the holiest rivers of Nepal and is revered by both Hindus and Buddhists. For Hindus it carries associations with sacred geography and salvation, and its banks are among the most important religious sites in the country. The river is central to the identity of the Kathmandu Valley and figures prominently in the valley's ritual life.

Its most famous stretch runs past the Pashupatinath Temple, the principal shrine of Lord Shiva in Nepal and a major Hindu pilgrimage destination, together with the nearby Guhyeshwari (Guheswori) Temple. The temple complex on the Bagmati is one of the country's most visited sacred sites and the focus of large festivals, most notably Maha Shivaratri.

The river is intimately bound up with Hindu death rites. Cremations are performed on stone platforms (ghats) along its banks, the most prominent being Arya Ghat beside Pashupatinath, where the deceased are traditionally cremated and their ashes committed to the river. By custom the body is dipped into the Bagmati before cremation, and the river is regarded as purifying and as aiding the soul's passage, reflecting the river's role in the cycle of life, death and liberation in Hindu belief.

Environment and hazards

Despite its sacred status, the Bagmati has become one of Nepal's most polluted rivers, especially through the Kathmandu urban area. Rapid, often unplanned urbanisation has loaded the river with untreated sewage and solid waste; large shares of the valley's wastewater have historically been discharged without treatment, and in the dry season the urban Bagmati can run as a heavily contaminated, low-flow channel. This degradation stands in stark contrast to its religious importance.

In response, restoration efforts have grown over the past decade. The Bagmati Cleanup Mega Campaign, launched in May 2013, has mobilised volunteers for regular Saturday clean-ups along the river over many years, operating largely on voluntary effort. Government bodies, including Kathmandu Metropolitan City, and basin-level programmes have also undertaken sewage interception, river-corridor improvement and flow-restoration measures, though restoring water quality and dry-season flow remains a major long-term challenge.

The river is also a significant flood hazard, a risk worsened by settlement and construction on its floodplains. During the September 2024 monsoon, exceptionally heavy rainfall over the Kathmandu region drove the Bagmati well above its danger level, contributing to severe flooding in parts of the capital and across the wider valley. The wider 2024 floods and landslides across Nepal caused very heavy loss of life nationwide, with the Kathmandu Valley among the hard-hit areas. Analysts have linked the scale of the disaster to record rainfall, climate change and rapid urban encroachment onto the river's floodplain.

At a glance

Key facts

TypeRiver (rain- and groundwater-fed, non-glacial)
SourceBaghdwar spring, Shivapuri hills, near Sundarijal, Kathmandu Valley (approx. 2,740 m / 8,990 ft)
LengthApproximately 586 km (about 364 miles)
Major tributariesBishnumati, Manohara, Dhobi Khola (Rudramati), Tukucha; lower basin: Marin Khola, Lakhandei, Lalbakaiya
OutflowJoins the Kamala River in Bihar, India; ultimately part of the Ganges (Ganga) system
CitiesFlows through the Kathmandu Valley, historically separating Kathmandu and Patan (Lalitpur)
Key sacred sitesPashupatinath Temple, Guhyeshwari Temple, Arya Ghat cremation ghats
Major irrigation useBagmati Irrigation Project via Bagmati Barrage, Karmaiya (Sarlahi and Rautahat districts)
Notable recent floodSeptember 2024: river rose roughly 2.2 m above its danger mark amid record Kathmandu-region rainfall

Main tributaries

BishnumatiManoharaNakkhuKulekhani (Indra Sarovar)
Loading map…

The Bagmati (highlighted) shown with the rest of the Southern / Mahabharat system. Real river courses from OpenStreetMap — hover to label, click to switch river.

The power it holds

Hydropower on the Bagmati

6 catalogued plants on or fed by this river, 170 MW in total. Tap any plant for its full profile.

PlantCapacityStageDistrict
Kulekhani I Hydropower Station60 MWOperationalMakwanpur
Super Tallo Bagmati Hydroelectric Project41 MWUnder constructionLalitpur
Kulekhani II Hydropower Station32 MWOperationalMakwanpur
Bagmati Khola Hydropower Project22 MWOperationalMakwanpur
Kulekhani III Hydroelectric Project14 MWOperationalMakwanpur
Sundarijal Hydropower Station0.97 MWOperationalKathmandu

More in the Southern / Mahabharat group

Common questions

Bagmati: frequently asked questions

How long is the Bagmati?+

The Bagmati is about 195 km long. ≈195 km in Nepal; ≈586 km in total to its outfall in Bihar (Wikipedia).

Where does the Bagmati start?+

The Bagmati rises at The Bagdwar springs in the Shivapuri hills, north of Kathmandu. It empties at Crosses into India and joins the Koshi/Ganga in Bihar.

Which river system does the Bagmati belong to?+

The Bagmati is part of the Southern / Mahabharat group of southern rivers. Spring- and rain-fed, rising in the Middle Hills.

What are the main tributaries of the Bagmati?+

Its main tributaries include Bishnumati, Manohara, Nakkhu, Kulekhani (Indra Sarovar).

What hydropower is built on the Bagmati?+

6 catalogued hydropower plants are on or fed by the Bagmati, totalling 170 MW. The largest is Kulekhani I Hydropower Station at 60 MW in Makwanpur.