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Bhutan: glacial flood

Active situation ·Glacial lake outburst flood

Active situation. Being tracked now. The figures are still moving.

Bhutan ·30 Oct 2026

15,000 Displaced or evacuated Preliminary Outlets report 10,000–15,000 · 6 sources

Why this keeps happening

What is a GLOF

A flood with no rain in it.

Picture a bucket made of ice and loose rubble, parked high on a mountain. The glacier left it there when it melted back, and it has been filling with meltwater ever since. Nobody built it. Nothing holds it but the rubble.

Now global heating — heating, not warming — thins the ice binding that rubble together. The walls were never strong. They are getting weaker.

Then something falls in. A slab of rock. A wall of ice. The bucket empties down the valley all at once, and it does it in minutes.

By the time anyone downstream knows, it is already there.

The numbers we cannot ignore

The geography of this risk is already mapped. What follows is what has been counted, and by whom.

28,043 Glacial lakes mapped across the Indian Himalayan river basins Official estimate ISRO / NRSC
63,000 Glaciers across the Hindu Kush Himalaya Official estimate ICIMOD
25,614 Glacial lakes mapped across the Hindu Kush Himalaya Confirmed ICIMOD
2,485above 10 ha Glacial lakes CWC monitors Confirmed Central Water Commission
15 million People exposed worldwide Confirmed Nature Communications
1,203 → 2,963 Lakes at high or very high risk, now and by 2100 Confirmed Nature Climate Change

The danger is not a distant hypothetical. The question is whether monitoring, planning and construction follow what is already known.

And they are not separate hazards. This is one chain.

  1. Warming and glacier retreat
  2. Unstable ice, rock and slopes; glacial lakes forming and expanding
  3. A trigger — extreme rain, avalanche, landslide or earthquake
  4. River blockage, or a lake outburst
  5. Debris flow and flash flood
  6. Roads, bridges, hydropower and towns in the path
  7. Mass casualties, tens of kilometres downstream

Flood, landslide, cloudburst, avalanche, outburst — described one at a time, they look like separate accidents. They are a sequence, and it is why assessment project by project cannot see what arrives catchment by catchment.

What science can say

Climate change does not pull every trigger, but it is loading the system: glaciers retreat, new lakes form and existing ones expand, moraine dams and frozen rock lose their binding, and slopes become less stable. Across the Third Pole, outburst risk is projected to roughly triple by 2100 — with ICIMOD's own caveat that a higher hazard has not yet produced a higher rate of floods.

What has not been attributed

Nobody has established that climate change caused THIS event. Single-event attribution takes months, and for a glacier or rock collapse it is often not possible at all. A rising hazard across a region is not a finding about one flood in it.

All 16 standing figures for this hazard, and their sources

A glacial lake outburst is a flood with no rain in it. Meltwater collects behind a moraine or an ice dam, something displaces it — a rockfall, an avalanche, a thaw — and the dam fails in minutes. The Himalaya holds tens of thousands of these lakes, India monitors a fraction of them, and the warning systems are almost entirely unbuilt.

28,043 — Glacial lakes mapped across the Indian Himalayan river basins. Lakes above 0.25 ha. THE BASINS, NOT THE TERRITORY: these river basins extend into Pakistani, Chinese and Nepali ground, so this is not a count of lakes inside India and is routinely quoted as though it were. ISRO / NRSC

63,000 — Glaciers across the Hindu Kush Himalaya. The source region for river systems supporting billions of people. ICIMOD

25,614 — Glacial lakes mapped across the Hindu Kush Himalaya. A 2005 Landsat baseline, not a current count — lakes have grown and formed since, so this understates today's number. India's own basin atlas counts 28,043 lakes above 0.25 ha, but across whole river basins including Pakistani, Chinese and Nepali territory, so it is not a count of lakes in India. ICIMOD

2,485 above 10 ha — Glacial lakes CWC monitors. Plus 358 other water bodies, monitored June to October on Sentinel imagery. The portfolio grew from 902 in 2025. Of these, 681 glacial lakes lie inside India: Arunachal 324, Ladakh 179, Jammu & Kashmir 76, Sikkim 72, Himachal 17, Uttarakhand 13. Central Water Commission

15 million — People exposed worldwide. Living BOTH within 50 km of a glacial lake AND within 1 km of a potential flood path — the two conditions together, which is the part most often dropped in quotation. India holds the largest exposed population of any country, about 3 million. India leads on exposure; on the study's danger index, which weights vulnerability, China and Pakistan rank higher. Nature Communications

1,203 → 2,963 — Lakes at high or very high risk, now and by 2100. Outburst risk across the Third Pole is projected to roughly triple, with the eastern Himalaya — the transboundary basins above Bihar and Bengal — remaining the primary hotspot under every scenario. Nature Climate Change

766 events, 1533–2025 — Recorded outbursts across High Mountain Asia. About 59 of them in India, per the peer-reviewed version of the database. ICIMOD's own caveat: the record is an underestimate, and the apparent rise over time is mainly better observation rather than more events. ICIMOD

+65% — Glacier mass loss, one decade against the last. From −0.17 to −0.28 metres water equivalent a year, between 2000–2009 and 2010–2019, with high confidence. Losses are steepest in the eastern Himalaya. ICIMOD

none — End-to-end warning systems commissioned in India. The government's own position as of 2026, under a ₹150 crore four-state programme approved in July 2024, of which ₹27.73 crore of ₹135 crore had been released by mid-2025. Two automatic weather stations are confirmed installed, in Sikkim. Press accounts describing twenty or more instrumented lakes contradict the government's own answer. Ministry of Home Affairs / NDMA

189 — High-risk glacial lakes assessed across the Indian Himalayan Region. From the 2025 assessment. India's National Disaster Management Authority separately lists 195 high-risk lakes; the two exercises are not the same and this page prints both rather than choosing between them. 2025 assessment, Indian Himalayan Region

56 — Of those, classified VERY HIGH RISK. The same figure a 2026 parliamentary reply gave for the highest risk class. 2025 assessment, Indian Himalayan Region

9 — Potentially dangerous glacial lakes in the Alaknanda Valley. The highest concentration in Uttarakhand, and the valley carrying the road to Badrinath. The Dhauliganga Valley follows with 6. 2025 Uttarakhand valley assessment

713 — Glacial lakes in Chamoli district alone. The highest concentration of any Uttarakhand district in this inventory. Chamoli is where the 2021 rock-ice avalanche happened. ISRO / IIRS

25 — Potentially dangerous, of 426 larger Uttarakhand lakes assessed. Six of the 25 fall in the most hazardous class, Category A. 2025 Uttarakhand valley assessment

1,200-1,350 — Glacial lakes identified in Uttarakhand. The range is real: the count depends on which inventory and which minimum size threshold is used. ISRO / IIRS

195 — Lakes on India's high-risk list. Himachal 48, Sikkim 41, Ladakh 34, Arunachal 32, Jammu & Kashmir 27, Uttarakhand 13. By type, 103 are moraine-dammed. A 2026 parliamentary reply put 56 of them in the highest risk class. National Disaster Management Authority

Figures in circulation that do not hold up

  • 'About 200 glacial lakes in the Hindu Kush Himalaya are dangerous' — the figure appears in an ICIMOD press release but nowhere in the report it is attributed to, and its likely ancestor is an inventory built partly on topographic maps from 1960–1982.
  • '178 dead at South Lhonak' — contradicted by every readable source; the disputed range runs from 55 dead with 74 missing to about 102.
  • 'India has the highest GLOF danger in the world' — India has the highest exposed population. On the danger index, which weights vulnerability, China and Pakistan rank above it.
  • '67 Indian glacial lakes have expanded by more than 40%' — absent from the ISRO page it is attributed to. ISRO's published finding is that 130 lakes in India expanded notably since 1984.
  • '47 potentially dangerous glacial lakes in Nepal' — the 47 is a three-country figure. Nepal's share is 21, China's 25 and India's 1.

Where

Bhutan — and the river it runs into. Positions are real coordinates; the extent of the event is not known.

The area the satellite frames cover Koshi — in the path downstream Bihar — in the path downstream Assam — in the path downstream West Bengal — in the path downstream Bhutan Bhutan Koshi Bihar Assam West Bengal

Region named in the reportingDownstream, in the pathThe satellite frame

Frame 1,117 km wide. The ring is an area, not a point: the reporting names the region, not a location inside it. Positions of the downstream places are true.

  1. Origin Glacial lake, high Himalaya
  2. Direct impact Moraine dam fails
  3. In the path Headwater river
  4. Downstream Koshi / Gandak / Brahmaputra
  5. Under watch Bihar, Assam, north Bengal

Upstream of India — shared river system Bhutan’s rivers feed the Brahmaputra through Assam and West Bengal.

What caused it

Candidate mechanisms, each with the evidence word it has actually earned and, where one exists, the counted thing that makes it plausible. Nothing on this list is established for this event.

Under investigation Glacial lake breach A moraine-dammed lake failing and draining in minutes. 766 events, 1533–2025 Recorded outbursts across High Mountain Asia ICIMOD
Under investigation Ice or rock avalanche A collapse into the lake, or a debris flow with no lake in it at all. +65% Glacier mass loss, one decade against the last ICIMOD
Under investigation Extreme rainfall Rain overtopping the dam, or a cloudburst producing the flood by itself.
Under investigation Landslide blockage and collapse A slide dams the river, the blockage fills, and then it fails.
Not established Thawing permafrost Frozen debris holding the dam together losing its ice.
How would we know?
Glacial lake breach
The lake, before and after. An emptied lake shows at 10 m, and the area change is measurable — usually settled within days of the first clear pass.
Ice or rock avalanche
A detachment scar on the slope above, and seismometers, which time a rock-ice collapse to the second. This is how Chamoli 2021 was reclassified.
Extreme rainfall
Gauge or radar rainfall in the hours before. A true outburst has no rain in it, so a heavy-rain record is evidence AGAINST one.
Landslide blockage and collapse
A temporary lake upstream, and a discharge record that rises, falls, then rises higher. Often established only after the second flood.
Thawing permafrost
Ground temperature and modelling of the slope. A condition rather than a trigger — it was the finding at Sikkim in 2023.

The mechanism in general

Trigger
A rockfall or avalanche into the lake, a surge over the moraine, or permafrost loosening the debris behind it. Minutes long, and no rain in it.
Conditions
Retreating glaciers leave meltwater ponded behind loose moraine, never engineered. Himalayan mass loss rose 65% from the 2000s to the 2010s, so the lakes are more numerous, larger and younger.
What science says
Outburst risk across the Third Pole roughly triples by 2100, high or very high risk lakes going from 1,203 to 2,963. ICIMOD's caveat: higher hazard has not yet produced more floods.
Human factors
What was built in the path decides the disaster. Sikkim 2023 destroyed a 1,200 MW dam and about 25,900 buildings on the Teesta. Nepal's Bhote Koshi warning gives roughly six minutes, its sensors all below the border the water starts above.

The mechanism for this kind of event, not a finding about this one. Himalayan disasters are often reclassified once fieldwork is done.

What the satellite sees

Imagery published here, not linked to. The same public NASA layers a newsroom would use, over the region the reporting names, on the dates either side of the event.

The same region before the event, 2026-10-27
The same region after the event, 2026-10-30
Before · 2026-10-27 After · 2026-10-30

Drag to wipe. Same layer, same box, same satellite. Cloud 0.9% before, 72.2% after.

Frame 24.91–30.11°N, 87.499–93.361°E. The region reported, not a located site.

Open the live comparison Zoom, re-date, or switch to radar.

NASA Worldview Snapshots. Public domain, courtesy of NASA EOSDIS GIBS.

It has happened before

4 comparable events, with what each one actually cost. Every toll below is an official or peer-reviewed count, not a headline.

2023 South Lhonak Lake, Sikkim 55 dead, 74 missing and other credible counts run to 102; there is no settled figure Official estimate Science
2013 Chorabari Lake, above Kedarnath 169 confirmed, 4,021 missing for the whole June 2013 Uttarakhand floods; the state later put it above 6,000, and no final count exists Official estimate National Institute of Disaster Management
1985 Dig Tsho, Nepal 4 or 5 deaths — the figure of twenty or more in circulation is unsourced Official estimate ICIMOD
2021 Chamoli, Uttarakhand — and not a GLOF 204 missing, presumed dead Official estimate Science
What happened in each, and what was learned
South Lhonak Lake, Sikkim · 3–4 October 2023
South Lhonak Lake, Sikkim. 14.7 million m³ of frozen moraine collapsed into the lake, raising a wave around 20 m high that breached the dam and released some 50 million m³ of water. It destroyed the 1,200 MW Teesta-III dam at Chungthang and travelled 385 km down the Teesta into Bangladesh, damaging about 25,900 buildings and 31 major bridges. There was no functioning early warning system; what warning reached people came informally from border police upstream.
Chorabari Lake, above Kedarnath · 16–17 June 2013
Chorabari Lake above Kedarnath, Uttarakhand, overtopped its moraine and drained in five to ten minutes — the second phase of the disaster, after a rainfall-driven debris flow the day before. A genuine lake outburst, though the lake was rain-fed rather than glacier-fed.
Dig Tsho, Nepal · 4 August 1985
Dig Tsho, Nepal. An ice avalanche into the lake overtopped and cut the end moraine; six to ten million m³ drained in about four hours, destroying a nearly-complete hydro plant 11 km downstream and 14 bridges. It struck during a lull in the trekking season.
Chamoli, Uttarakhand — and not a GLOF · 7 February 2021
Chamoli, Uttarakhand — commonly filed as a glacial lake outburst and not one. About 27 million m³ of rock and glacier ice fell from Ronti Peak and became a debris flow. No lake was involved; the peer-reviewed account was written specifically to correct the early reporting.

What these counts leave out

  • Lakes below the monitoring threshold. CWC monitors above 10 hectares; the July 2025 Rasuwa flood came from a supraglacial lake in Tibet that had not been noticed at all.
  • Anything upstream of the border. India has no gauge above the Tibetan frontier on the Brahmaputra system, and Nepal's Bhote Koshi warning system has a lead time of about six minutes because its sensors are all on the Nepali side of a catchment that begins in Tibet.
  • The distinction between hazard types, in early reporting. Rock-ice avalanches, landslide-dam breaks and true lake outbursts are routinely reported as one another in the first days, and the correction usually arrives months later in a journal.

The alarm for India

Nepal is not somebody else’s disaster. The triggers differ; the vulnerability is the same, and it is already measured.

Confirmed India impact

No named source has reported an Indian casualty or evacuation figure.

What is already counted above India

none End-to-end warning systems commissioned in India Ministry of Home Affairs / NDMA
189 High-risk glacial lakes assessed across the Indian Himalayan Region 2025 assessment, Indian Himalayan Region
56 Of those, classified VERY HIGH RISK 2025 assessment, Indian Himalayan Region
9 Potentially dangerous glacial lakes in the Alaknanda Valley 2025 Uttarakhand valley assessment
713 Glacial lakes in Chamoli district alone ISRO / IIRS
25 Potentially dangerous, of 426 larger Uttarakhand lakes assessed 2025 Uttarakhand valley assessment
1,200-1,350 Glacial lakes identified in Uttarakhand ISRO / IIRS
195 Lakes on India's high-risk list National Disaster Management Authority

The corridors this maps onto

Alaknanda 9 potentially dangerous glacial lakes, the highest concentration in Uttarakhand. Carries the road to Badrinath, major settlements, pilgrimage infrastructure and hydropower. 2025 Uttarakhand valley assessment
Dhauliganga 6 potentially dangerous lakes, second in Uttarakhand. 2025 Uttarakhand valley assessment
Chamoli district 713 glacial lakes, the highest of any Uttarakhand district, with population, roads and pilgrimage routes downstream of high-altitude catchments. ISRO / IIRS
Bhagirathi and Mandakini Glacier-fed valleys with the same combination of high hazard and dense seasonal use. 2025 Uttarakhand valley assessment

Downstream of this event: Bihar and eastern Uttar Pradesh on the Koshi and Gandak; Assam and north Bengal on the Brahmaputra and Teesta. The Koshi basin is 2.6% of the Himalaya's southern slope and has produced 51.6% of its recorded glacial lake outbursts.

This column is exposure, not an outcome. Nothing in it is a report that anything has happened in India. It is where the same hazard would arrive.

What happens next

Two horizons. A level only where a published threshold and a number exist to put something against — everything else is named as a watch, not graded.

Next 24–72 hours

Low More rain over the region Peak 21.7 mm in one day across the next 3, against IMD's heavy-rainfall threshold of 64.5 mm and very heavy at 115.5 mm.
Watch The mechanism confirmed Chamoli 2021 was called a glacier burst and was a rock-ice avalanche.
Watch A second surge The river was blocked once and released. A blockage that refills can fail again, larger.
Watch River levels downstream Central Water Commission gauges, and whether any cross a warning mark.
Watch Emergency mapping activated Copernicus would give the first authoritative extent maps.
Watch The casualty count settling Early Himalayan counts move by an order of magnitude in the first week.

Coming days and weeks

Watch Sediment moving downstream The 2023 Teesta flood was traceable 385 km, into Bangladesh.
Watch Slopes failing again Valley walls a debris flow has cut are the next monsoon's landslides.
Watch Roads out for a season In a Himalayan valley that is the supply route, not only the tourist one.
Watch Displacement that does not reverse Villages in a newly-cut channel are not rebuilt in the same place.
Watch Hydropower rebuilt on the same assumptions What was in the path, put back where it was.

The rainfall level is computed from a forecast model over a representative point — Open-Meteo forecast API, not a gauge at the event. The ungraded items are the mechanisms that follow this hazard. This page does not pretend to know their probability.

Data and sources

Everything this page is built from, counted by kind. Nothing here is quoted in this site’s own voice.

27 published reports
81 independent publishers
View all 27 sources

Reported

A headline is evidence that something was said. It is never evidence that it is true — which is why every figure at the top of this page carries the outlet that printed it and, where they disagree, all of them.

What is not established
  • Casualty and damage figures are not established here. Any number in the headlines below belongs to the outlet that printed it.
  • The mechanism is this page's reading of how the event was first reported, not a finding. Himalayan disasters are often reclassified once fieldwork is done.
  • The extent of the affected area has not been verified against satellite or official mapping.
  • Downstream consequences for India are a known mechanism for this hazard, not a confirmed outcome of this event.

Last changed 14:39 IST, 30 Oct 2026.

This is one event

The standing picture — how much extreme rain India actually gets, what IMD counts as extreme, who the rain kills, and what is changing across twelve cities — is on the situation page this belongs to.

India’s extreme rain

A gap is a gap

An empty day stays empty — a gap in the record is a gap in the record, never a zero.

Cite this page

Reuse freely — CC BY 4.0. Every figure carries its source and its cadence in how the number is made. If you quote a number from here, quote the kind with it. Each upstream source keeps its own terms.

This is what we are doing.
It is not enough.

The work against this reading

Mostly the written record, and going to look. Three of the essays on this site were reported out of flood years, and Gram Anubhav takes groups into villages living with this, run with over a hundred grassroots partners in the villages themselves.

And why it is not a reply

Publishing and going to see are not resilience. Swechha does not build drainage, and nothing here reduces the 3,594 deaths this page counts. What the work does is make the count harder to ignore — a smaller claim than it sounds, and the only one the evidence supports.

Once a month, what these numbers did.

One email. What the six readings did that month, what moved and what did not, and what we did about it. Nothing else, ever — no appeals between digests, and your address is never shared with anybody.

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