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The Kosi: why it is called the Sorrow of Bihar

No river in India has shifted its course as dramatically as the Kosi — westward by well over a hundred kilometres in two centuries. In August 2008, it broke through its embankment at Kusaha in Nepal and flooded vast areas of north Bihar. The science of the Kosi, the history of controlling it, and what a better approach looks like.

17 Oct 2026 4 min read

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In this guide
  1. The river
  2. Why the Kosi is so difficult
  3. The Kosi project
  4. The embankment debate
  5. The 2008 Kusaha breach
  6. Options for the future
  7. Why the Kosi matters for BPSC
  8. Practice

On 18 August 2008, the Kosi broke through its eastern embankment at Kusaha in Nepal, a few kilometres upstream of the barrage at Bhimnagar. The river abandoned its channel and poured into an old course to the east, flooding districts such as Supaul, Madhepura, Saharsa, Araria and Purnia. Lakhs of people were displaced; villages, roads and fields disappeared under water and sand. It was one of the worst disasters in Bihar's recent history — and a reminder of why the Kosi is called the Sorrow of Bihar.

The river

  • The Kosi is formed in Nepal by seven Himalayan streams — hence Sapta Kosi — including the Sun Kosi, Arun and Tamur. Its catchment includes some of the world's highest peaks, including the Everest region.
  • It enters Bihar near Bhimnagar (Supaul district) and flows south to join the Ganga near Kursela (Katihar district).

Why the Kosi is so difficult

FactorExplanation
Enormous sediment loadThe Kosi carries one of the highest sediment loads of any river in the world, from the young, easily eroded Himalaya
Sudden drop in gradientWhen it leaves the steep mountains and enters the flat plain, the river slows and drops its sediment
AggradationSediment raises the riverbed, so the river spills over its banks
Shifting courseThe river repeatedly abandons its raised bed for lower ground
Heavy monsoon rainIn the Nepal catchment, rainfall is intense and concentrated
Seismic zoneThe region is earthquake-prone, which affects slopes and sediment supply

The Kosi megafan

Over thousands of years, the shifting Kosi has built a huge, fan-shaped deposit of sediment — the Kosi megafan — one of the largest in the world. Over roughly the last two centuries, historical maps show the river shifting westward by well over a hundred kilometres across this fan.

The Kosi project

After independence, India and Nepal signed the Kosi Agreement in 1954. The Kosi project included:

  • the Kosi barrage at Bhimnagar (on the Nepal border), completed in the early 1960s;
  • embankments on both sides of the river to confine it to a fixed channel;
  • canals for irrigation (the Eastern and Western Kosi canals);
  • a small hydropower component.

The embankment debate

Embankments did stop the Kosi from shifting for decades. But experts have long pointed to problems:

ProblemExplanation
Silt trapped between embankmentsThe riverbed rises between the embankments, sometimes above the surrounding land
Villages inside the embankmentsSeveral hundred villages lie between the embankments, flooded almost every year, with poor services
Waterlogging outsideEmbankments block natural drainage, causing waterlogging in the countryside outside
BreachesWhen an embankment breaks, the damage is catastrophic, because water rushes into areas that have grown complacent — as in 2008
MaintenanceMaintaining long embankments on shifting sands is difficult and costly

Researchers and activists such as Dinesh Kumar Mishra have documented these problems in detail.

The 2008 Kusaha breach

  • Cause: a breach in the eastern embankment at Kusaha, in Nepal — attributed to weaknesses in the embankment and inadequate maintenance and monitoring, at a time of relatively moderate flow.
  • Effect: the river took an old course to the east, flooding large parts of north-east Bihar.
  • Response: major rescue and relief operations; later, reconstruction under the Kosi Flood Recovery Project with World Bank support.
  • Lessons: the importance of maintenance, monitoring, early warning, and cooperation with Nepal.

Options for the future

OptionProsCons
High dam in Nepal (the proposed Sapta Kosi High Dam)Could store water, trap sediment, generate power and control floodsVery costly; seismic risk; displacement in Nepal; sediment would fill the reservoir; needs agreement with Nepal
Stronger embankmentsProtects existing investmentsDoes not solve siltation
Living with floodsFlood-resilient housing, raised platforms, early warning, flood insurance, floodplain zoningRequires changes in settlement and livelihoods
Drainage improvementReduces waterloggingNeeds sustained investment
Sediment managementDredging; allowing controlled flooding to spread siltTechnically challenging
River linking (Kosi–Mechi)Diverts waterLimited effect on floods; costly

Most experts now favour a flood management approach — reducing losses and helping people live with floods — rather than only trying to control the river.

Why the Kosi matters for BPSC

  • It is a classic Prelims and Mains topic.
  • It links geography (sediment, megafans), disaster management (2008), international relations (India–Nepal agreements), economy (the Kosi region is among Bihar's poorest) and migration.

Practice

Prelims-style:

  1. Why is the Kosi called the Sapta Kosi?
  2. When was the Kosi Agreement signed with Nepal?
  3. Where is the Kosi barrage?
  4. Where did the 2008 breach occur?
  5. In which direction has the Kosi shifted over the last two centuries?

Mains-style:

  • "Embankments have turned the Kosi from a problem into a disaster." Critically examine.
  • Suggest a sustainable strategy for managing floods in the Kosi basin.

A note on dates and numbers. Exam patterns, vacancies and schedules change from year to year. Always confirm the current details in the latest notification on the Bihar Public Service Commission website .

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