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Himalayan Glacier Disaster Timeline (2021–2026): Nepal–Tibet Flood, GLOFs & Rising Mountain Risks

📅 Updated 22 September 20265 major events trackedChamoli · Sikkim · Thame · Rasuwa · Nepal–Tibet
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Himalayan glacier disasters from Chamoli to the 2026 Nepal-Tibet flood: GLOFs, ice-rock avalanches, the USGS earthquake correction and the climate link.

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The flood arrived from a place where it was not raining. High in the Himalayas near the Nepal–Tibet border, a mass of glacier ice, rock and sediment broke away on 26 August 2026 and plunged roughly 1,200 metres into the valley below. The collapse generated a seismic signal strong enough to be mistaken at first for an earthquake — then the disaster changed form, blocking a river and sending a violent mixture of water, mud, ice and rock down the Lhende Khola, Bhote Koshi and Trishuli valleys. That sequence is the reason Himalayan glacier disasters are so hard to prepare for: the thing that starts the disaster is often not the thing that kills people downstream.

Himalayan Glacier Disaster Timeline (2021–2026): Nepal–Tibet Flood, GLOFs & Rising Mountain Risks

Fact-checked: 22 September 2026. The 2026 Nepal–Tibet event’s death toll has risen sharply since the collapse and remains under investigation — numbers below carry a source and a timestamp. Scientific mechanism for each older event follows the latest peer-reviewed study or ICIMOD analysis, not the first breaking-news description.

Latest Update — September 2026

Nepal’s disaster authority sharply revised the missing-persons count upward on 16 September 2026, after renewed data collection and cross-checking with district offices: the toll jumped from 5,179 reported the day before to 6,150 missing, alongside 1,403 bodies recovered (105 identified so far), spokeswoman Shanti Mahat told AFP. By 18 September 2026, Nepal’s confirmed death toll had risen further to 1,410, with 6,145 still listed missing and 9,287 injured — a small net revision as verification work continued rather than a new wave of casualties (AFP via Webindia123, 18 September 2026). The same 16 September figures put Nepal’s injured count at 9,287 and confirmed 607 foreign nationals from 34 countries remained among the missing there — including 189 Indians, 65 Americans, 55 Malaysians and 32 Britons — while a further 261 foreign nationals from 23 countries were listed missing on the Tibet side, per Nepal’s disaster authorities. China’s state media continued to report 43 dead and 519 missing in Tibet as of 6 September, putting the combined toll at roughly 1,446 dead and 6,669 missing (AFP via Philstar, Jamaica Observer, Courthouse News, 16–17 September 2026). Officials attributed the jump to fuller verification rather than a new wave of casualties. Earlier, as of 12 September 2026, Nepal’s disaster authorities had put the toll at 1,386 dead, 5,130 missing and 6,827 injured in Nepal, with a further 43 dead and 519 missing in Tibet (as of 6 September); the missing count had held steady at 5,130 for a second day as remaining search efforts shifted to identifying the roughly 1,282 recovered bodies not yet matched to families (Kathmandu Post, 12 September 2026). Attention has shifted to paying for the recovery: a Rapid Damage and Needs Assessment released by the Prime Minister’s Secretariat on 10 September 2026 — prepared jointly by the National Planning Commission and the National Disaster Risk Reduction and Management Authority — puts total reconstruction and recovery needs at Rs 723.315 billion (about US$4.74 billion). Infrastructure accounts for roughly 75% of that, about US$3.1 billion, with the energy sector the hardest hit — 13 hydropower projects totalling around 759 MW plus five solar plants were damaged; about Rs 8.7 billion is needed over the next six months for immediate relief and Rs 714.58 billion for long-term rebuilding. A fuller Post-Disaster Needs Assessment is still to follow. As of 21 September 2026, Nepal’s government signalled it will skip the formal donor-conference model used after the 2015 earthquake in favour of bilateral negotiations with individual donor countries — India, China, the US, Japan, South Korea and European nations among them — with Finance Minister Swarnim Wagle pursuing commitments on visits including Doha, New York and Washington DC through September–October 2026 (Kathmandu Post, 21 September 2026). Nepal says it prefers grants but that loans “may be unavoidable.” On 26 September 2026, Wagle left for Doha to attend the 11th annual meeting of the Asian Infrastructure Investment Bank’s Board of Governors on 28–29 September, where he plans to meet counterparts from India, China, Bangladesh and the Maldives and the AIIB chairman to seek support for post-flood reconstruction — still costed at around US$5 billion over three to five years — before heading to the IMF–World Bank annual meetings in Bangkok in October (Kathmandu Post, 26 September 2026). At a meeting in Doha reported on 28 September 2026, AIIB President Zou Jiayi pledged grant assistance for project preparation through the bank’s Project Preparation Special Fund and said loans could be kept at the most concessional rate possible by blending in grants from its Special Fund window; Wagle also sought faster studies on power-distribution and expressway projects, but no loan or grant amount was announced (Nepal News; OnlineKhabar, 28 September 2026). On climate finance, two separate threads are running: Nepal has already secured US$20 million from the UN-backed Fund for Responding to Loss and Damage under the Barbados Implementation Modalities — approved from three proposals filed before the flood, and not yet disbursed pending reviewer sign-off — while a separate emergency request filed on 31 August 2026 specifically for Bhotekoshi flood relief remains undecided; the Fund’s board co-chairs said on 10 September 2026 they were working to address it “as rapidly as possible,” with a developing-countries constituency meeting set for 12 September ahead of a board meeting now expected before its originally scheduled December date (Kathmandu Post, 9–10 September 2026). Separately, the Green Climate Fund’s $36.1 million “GLOF Sanjeevani” project to drain four unrelated high-risk lakes — Thulagi, Lower Barun, Lumding Tsho and Hongu 2 — remains only about 26% disbursed as of early September 2026, per the Kathmandu Post (6 September 2026). Infrastructure tallies are also coming into focus: Nepal’s Department of Roads says the flood destroyed roughly 40 km of the Galchhi–Rasuwagadhi highway and 41 motorable bridges, putting road and bridge damage alone at about Rs 30 billion (full rebuild near Rs 50 billion), with officials aiming for temporary Bailey-bridge connectivity to the Chinese border by the Dashain festival in October (Kathmandu Post, 13 September 2026). Nepal’s National Disaster Risk Reduction and Management Authority’s 21 September 2026 update put the Nepal toll at 1,451 dead and 5,786 missing (including 636 foreign nationals) — the missing count falling from 6,145 on 18 September as identification work reclassified some of the unaccounted — with roughly 13,784 people rescued and more than 20,900 security personnel still deployed in search and recovery operations (NDRRMA, via Qazinform, 21 September 2026). A month after the flood, NDRRMA figures reported on 26 September 2026 put Nepal’s toll at 1,453 dead (1,451 bodies recovered plus two people who died in treatment) and 5,285 missing, with 13,795 people rescued; only 112 bodies have been identified and handed to families, as authorities match 1,329 DNA samples from remains against 2,060 from relatives, and 1,113 displaced people remain in 21 holding centres (NDRRMA via PTI/The Tribune, 26 September 2026). Fresh rain in late September has added to hardship in Rasuwa and Nuwakot camps, where displaced families report leaking tarpaulins and wet bedding; a Rasuwa district-level committee has identified potential resettlement land and sent recommendations to the central government, and NDRRMA chief executive Dharam Raj Uprety said detailed information has been collected on public and private land from Syaphrubesi and Timure in Rasuwa to Bidur in Nuwakot, with permanent-settlement options to be offered in safe locations — though no central decision had been announced (Kathmandu Post, 26 September 2026). Separately, a 14 September 2026 report by sustainability advisory Systemiq, with mountain-research partners including ICIMOD, found only 21 of an estimated 40,000 Hindu Kush–Himalaya glaciers are monitored on the ground and flagged about 200 glacial lakes in India as high-risk — 56 of them “very high risk” — warning that accelerating glacier melt is pushing the region toward “peak water” (Reuters via Kathmandu Post, 14 September 2026). Relief funding is running well behind reconstruction needs: the Prime Minister’s Disaster Relief Fund held about Rs 12.43 billion (roughly US$94 million) as of mid-September 2026, of which Rs 1 billion has been released to the NDRRMA for relief and rescue operations (Nepalnews, September 2026) — under 2% of the Rs 723.315 billion RDNA recovery estimate, underscoring why officials are pushing both the fuller Post-Disaster Needs Assessment and the planned donor conference. The government’s Rapid Damage and Needs Assessment, reported in detail by the Kathmandu Post on 15 September 2026, put total flood damage and economic losses at Rs 408 billion across the five worst-hit districts — Rasuwa, Nuwakot, Dhading, Gorkha and Chitwan — with the private sector absorbing nearly Rs 300 billion (more than two-thirds of the total), including an estimated Rs 146.19 billion in damage to almost 4,800 businesses and Rs 63.88 billion in damage to 7,570 private homes; the public sector’s share was about Rs 108 billion. Separately, the Kathmandu Post reported the same day that of 64 footbridges between Muglin and Timure along the Trishuli corridor, 53 were damaged — 20 needing repair and 33 requiring a full rebuild — with government work orders issued on 2 September 2026, five bridges under active repair as of mid-September, and officials targeting completion of the repairable spans within a month of that order. Nepal’s toll was revised again by 21 September 2026: NDRRMA put the count at 1,451 dead and 5,786 missing (including 636 foreign nationals) — missing falling from 6,145 on 18 September as DNA identification of recovered remains reclassified some of the unaccounted — with 13,784 people rescued, more than 20,900 security personnel still deployed, DNA samples collected from 530 unidentified bodies, and 1,231 displaced people sheltering at 20 holding centres (NDRRMA via Qazinform, 21 September 2026). Road crews were still 24 days from reconnecting Rasuwa and Nuwakot as of 19–20 September 2026: the 16 km stretch between Syabrubesi and Rasuwagadhi remained impassable to vehicles, with the Department of Roads assembling a Bailey-bridge fleet donated by China (two 100–metre spans), India (three 70–metre spans) and Nepal’s own Army and Department of Roads (three more 70–metre spans plus eleven shorter bridges up to 48 metres) across six washed-out crossings, still targeting the Dashain festival (second week of October) for a temporary link to the Chinese border (Kathmandu Post, 19–20 September 2026). Nearly a month on, the workplace toll is coming into sharper focus: Energy Minister Biraj Bhakta Shrestha told Parliament on 23 September 2026 that more than 800 hydropower and transmission workers remain unaccounted for, led by 439 still missing from the Upper Trishuli-1 project alone (of 1,433 on site when the flood hit, 955 rescued or contacted), plus 178 from Upper Trishuli-3B, 93 from Rasuwagadhi, 47 Nepal Electricity Authority staff and smaller numbers at five other sites — with search operations continuing (Kathmandu Post, 23 September 2026). The same day, the Asian Development Bank’s September 2026 Asian Development Outlook cut Nepal’s fiscal-year growth forecast to 4.1% (from 4.5% in July), raised its inflation forecast to 5.3% and projected the fiscal deficit widening to 4.7% of GDP (from a pre-disaster 3.4%), citing flood damage to transport, hydropower and farm output plus reconstruction spending (ADB, 23 September 2026). Also on 23 September 2026, the United States pledged a further US$31 million — $10 million for permanent bridges, $8 million for water, sanitation, shelter and livelihoods support, and $13 million for US-made recovery drones — taking total US flood-response funding for Nepal past US$36 million, per Under Secretary of State Allison Hooker (Kathmandu Post, 23 September 2026). The disaster also reached the UN General Assembly: opening its 81st session in New York on 22 September 2026, UN Secretary-General António Guterres recalled his 2023 warning from the Nepal Himalaya that “the rooftops of the world are caving in,” saying climate impacts are “arriving sooner, hitting harder, and spreading further than many anticipated” and that the biggest polluters “must do far more to repair the damage” (Kathmandu Post, Radio Nepal, 23 September 2026). Prime Minister Balendra Shah, on his first foreign trip since taking office, met Guterres and then addressed the Assembly on the night of 24 September 2026, calling the August flood “not just a local tragedy. It was a warning to the world,” and adding: “We did not create this crisis, yet we are paying a colossal price for it.” Citing at least 1,400 deaths, more than 6,000 still missing and recovery needs of roughly 10% of Nepal’s GDP, he proposed a Nepal–India–China Himalayan Climate Resilience Mechanism to share satellite data, monitor dangerous glacial lakes and strengthen early-warning systems, and called existing channels such as the Loss and Damage Fund and the Global Environment Facility inadequate, arguing Nepal cannot build resilience “through loans alone” (AP via US News, Kathmandu Post, 24–25 September 2026). In the same address he thanked Nepal’s neighbours, saying “India and China, offered prompt and generous assistance,” alongside the UN system, humanitarian agencies and other countries (ANI via The Tribune, Millennium Post, 25 September 2026). General Assembly President Khalilur Rahman had also referred to Nepal’s floods in his own statements at the session. Private giving has so far outpaced the multilateral channel: nearly US$90 million had been donated by individuals and companies to the Prime Minister’s Disaster Relief Fund, climate negotiator Manjeet Dhakal said on 21 September, while the Fund for Responding to Loss and Damage — with about US$820 million pledged, US$350 million earmarked for its first phase and a US$20 million per-project cap — had still not allocated money to Nepal’s 31 August emergency request, with its next scheduled board meeting beginning 15 December (Climate Home News, 22 September 2026). A Carbon Brief analysis published the same day found that Nepal’s US$20 million request would cover only about 0.7% of the roughly US$2.7 billion in estimated physical damage and economic losses (about 0.3% once US$4.8 billion in recovery costs are included), and that the Fund had received 176 requests totalling about US$2.8 billion — more than three times the roughly US$822 million pledged — while having paid out nothing as of September 2026; Nepal is its fourth-largest claimant (Carbon Brief, 22 September 2026). Identification remains the bottleneck: a month after the flood, only 112 recovered bodies had been returned to families and 2,035 DNA samples had been collected from relatives, while 54 of the 636 foreign nationals listed missing in Nepal were Ukrainian — most from a Mount Kailash pilgrimage group caught crossing back from Tibet — with families describing the search and identification process as “very slow” and destroyed immigration records complicating confirmation of who had crossed the border (OnlineKhabar, 25 September 2026). Schooling has also been hit hard: an Education Ministry assessment with UNICEF and Save the Children, published on 18 September 2026, found about 14,500 students at 63 institutions in Rasuwa, Nuwakot and Dhading affected, with 34 schools physically damaged (268 classrooms across 45 buildings) and 28 of 29 temporary holding centres operating from school buildings, delaying the return to class; the ministry is setting up 68 temporary learning centres (Kathmandu Post, 18 September 2026). At home, the flood risk has not passed: Nepal’s Meteorological Forecasting Division urged people to postpone long-distance travel from 25 to 27 September 2026 because of prolonged rainfall, naming settlements along the Sunkoshi, Bhotekoshi, Roshi, Khani and Bagmati rivers as particularly vulnerable, and authorities ordered the BP Highway in Kavrepalanchok closed at night from 24 to 28 September (Kathmandu Post, 23–24 September 2026). That warning proved justified: rainfall since 25 September killed at least 14 people across Nepal in 72 hours, including four each in landslides in Myagdi and Baglung districts, and the Narayani River crossed its 9-metre warning level, while fresh spells of rain reached Rasuwa and Nuwakot before flood-swollen rivers had fully receded, adding to hardship for families still sheltering under tarpaulins in temporary camps (ANI via The Tribune, 27 September 2026). By Sunday evening Nepal Police put the four-day rain toll at 15 dead, and the Narayani peaked at 11.94 m at Devghat against a 9 m danger level (Nepal News, 27 September 2026). The same weather system struck the high mountains: on the morning of 27 September 2026 an avalanche buried tents at the Himlung Himal base camp (7,126 m) in Manang district near the Tibet border; two Nepali guides’ bodies were recovered by helicopter and about a dozen expedition and kitchen staff remained missing, with reported counts ranging from 10 to 14 as heavy snow held up the search (Manang district officials via OnlineKhabar, 27 September; AFP/BBC via The Business Standard, 28 September 2026). Rescuers flown in by helicopter resumed the search on 28 September in clearer weather; Manang officials said the number still missing was unconfirmed because some workers earlier reported out of contact had walked to safety (Assistant CDO Krishna Prasad Poudel via Peoples’ Review, 28 September 2026). By 28 September four bodies had been recovered and identified — Chhebi Bhote and Pasang Bhote on 27 September, Birendra Gurung and Ghanshyam Rai on 28 September — and 12 people remained missing, with a Nepal National Mountain Guides Association team led by Mingma G Sherpa continuing the search (NNMGA President Tul Singh Gurung via Kathmandu Post/Asia News Network, 29 September 2026). In Doha, AIIB President Zou Jiayi told Finance Minister Swarnim Wagle the bank would give Nepal grant assistance for project preparation from its Project Preparation Special Fund and consider highly concessional loans for resilient reconstruction; no amount was announced (Nepal News and OnlineKhabar, 28 September 2026). NDRRMA’s own tally for the late-September rain, released on 29 September, counts 27 dead and 4 missing in 542 disaster incidents between 24 and 27 September — 20 of the deaths in landslides — with 227 houses destroyed and 31 bridges damaged; Dedhgaun in Nawalparasi East recorded the heaviest rainfall at 544.2 mm (NDRRMA via OnlineKhabar and Nepal Press, 29 September 2026). In Manang, a landslide on 27 September dammed the Marsyangdi River at Ghattekhola near Chame, impounding a lake roughly 400 m long; after a Nepal Army team found no suitable rock for blasting, the district deployed excavators on 29 September to cut a drainage channel, while power, water, telecom and road links in the area remained cut (Assistant CDO Krishna Prasad Poudel via OnlineKhabar; Peoples’ Review, 29 September 2026). On 29 September heavy snowfall halted the search at Himlung base camp, where four people are confirmed dead and 12 Nepali workers and guides remain out of contact; initial reports had listed 22 missing before rescuers reached 10 of them (Nepal National Mountain Guide Association officer Sovbit Kunwar via ETV Bharat, 29 September 2026). In an interview published the same day, NDRRMA chief executive Dharmaraj Upreti said the roughly 5,285 people still missing from the Bhotekoshi flood are being processed for legal declaration as deceased so families can receive relief of Rs200,000 per death, and that Nepal has begun a daily hydrological information exchange with China and gained access to RIMES satellite data for early warning (The Kathmandu Post, 29 September 2026). On reconstruction, Bagmati Province Chief Minister Kiran Thapa Magar on 29 September asked the other six provinces to help rebuild the 15 local units hit by the Bhotekoshi flood and said he would table a joint infrastructure proposal at the chief ministers’ meeting on 7–9 October (Nepal News, 29 September 2026). The AIIB annual meeting in Doha closed with Finance Minister Wagle elected a vice-chair of the bank’s Board of Governors for 2026–27, but still no reconstruction loan or grant amount (OnlineKhabar; Republica, 29 September 2026). On 30 September 2026 Nepal Police Headquarters put the Bhotekoshi flood count at 1,454 bodies recovered and 4,718 still missing, with 1,334 bodies managed after DNA sampling and 7,975 police personnel deployed; the police missing figure is lower than NDRRMA’s last published 5,285 (26 September) and the report does not explain the gap, so the tracker below keeps NDRRMA’s figures until the authority updates them (OnlineKhabar, 30 September 2026). The Energy Ministry says the 26 August flood damaged 14 hydropower projects totalling 783 MW, with an initial energy-sector damage estimate of Rs 134 billion; options under discussion for rebuilding include extending generation licences from 35 to up to 50 years and concessional loans, pending the National Planning Commission’s Post-Disaster Needs Assessment (OnlineKhabar, 30 September 2026). Separately, the Energy Ministry says the flood has cut about 430 MW from the national grid by disrupting Trishuli-corridor supply to Kathmandu’s Balaju and Chapali lines, and the Nepal Electricity Authority has formed a task force on alternative supply, including extra underground cabling, ahead of winter (spokesperson Mohan Kumar Shakya via OnlineKhabar, 30 September 2026). At Himlung base camp, rescuers recovered three more bodies on 30 September — Aash Gurung of Gorkha, Suraj Rai of Khotang and Kalam Budha of Rukum — bringing the avalanche toll to seven dead, with nine still missing (seven from Himalayan Holidays, two from Imagine Nepal); the bodies are to be flown to Kathmandu’s Teaching Hospital (Manang CDO Mukti Prasad Khanal via OnlineKhabar; Assistant CDO Krishna Prasad Paudel via Nepal News, 30 September 2026). A month after the flood, only about 1,000 of the roughly 4,500 people who first sheltered in temporary camps remain there, with many moving to rented rooms in Bidur and Kathmandu; none of the displaced families has yet received the promised Rs 15,000 a month for six months or the Rs 50,000 one-time settlement aid, because local units must first verify and recommend victims — Bidur Municipality alone has registered 1,536 displaced families (NDRRMA spokesperson Shanti Mahat via The Kathmandu Post, 30 September 2026). Returning from the UN General Assembly on 30 September, Foreign Minister Shisir Khanal said the United States and the United Arab Emirates had announced assistance for flood victims, without disclosed amounts, and that Nepal had pressed for simpler access to climate finance and the Loss and Damage Fund (The Kathmandu Post, 30 September 2026). As of 1 October, the direct Nuwakot–Rasuwa road link along the Galchhi–Syabrubesi corridor was still cut: road project chief Krishna Nath Ojha said a track being cut through a cliff should let vehicles reach the Phalaku Khola section by Friday (2 October), with 73-metre and 76-metre Bailey bridges planned there, while the Lamjung–Manang link also remained blocked; other flood-damaged highways, including the Prithvi and BP highways, had reopened to two-way traffic ahead of Dashain (The Kathmandu Post, 1 October 2026). On 1 October, search teams recovered eight more bodies near Himlung base camp — six flown by Nepal Army helicopter to Phu village and two to the district headquarters at Chame — raising the avalanche toll to 15 dead, with one of the 16 Nepali workers and support staff who were preparing the mountain’s routes and camps still missing (Manang Assistant CDO Krishna Prasad Poudel via OnlineKhabar and The Kathmandu Post, 1 October 2026). Also on 1 October, Infrastructure Minister Sunil Lamsal said a temporary track on the flood-damaged Galchhi–Betrawati road had reopened to public movement; the Nuwakot-side foundation for two Bailey bridges is ready and installation has begun with Nepal Army support, with the Rasuwa-side foundation in its final stage and completion targeted within a week (OnlineKhabar, 1 October 2026). By 2 October, foundations on both banks at Betrawati were complete and the bridge installation was under way, while long-term road reconstruction proceeds in parallel (Minister Lamsal via OnlineKhabar, 2 October 2026). Separately, the Ministry of Agriculture, Forest and Environment has circulated a draft National Climate Policy–2083 for comment ahead of COP31 in Türkiye in November; NGO Federation president Arjun Bhattarai said the government appeared to be rushing it on the pretext of the summit, and stakeholders want lessons from the Bhotekoshi flood built into it, while climate department head Maheshwor Dhakal said provincial consultations drew 700–1,000 people each (The Kathmandu Post, 1 October 2026). On 3 October, OnlineKhabar reported that the 37th meeting of the National Disaster Risk Reduction and Management Executive Committee had decided to continue search and rescue only in critical and highly sensitive locations while prioritising recovery of bodies and damaged structures elsewhere, with 5,285 people still listed as missing; Langtang Khola Hydropower Project manager Bijay Mohan Bhattarai said about a kilometre of road beyond Chilime was destroyed and that restoring access to some Rasuwa projects, including Chilime, Langtang and Rasuwagadhi, could take up to a year (OnlineKhabar, 3 October 2026). NDRRMA executive chief Dharmaraj Upreti had announced the move from search-and-rescue to search-and-recovery at a Singha Durbar press conference on 30 September, alongside a three-step verification of missing persons — certified by local governments, verified by District Administration Offices, then processed by NDRRMA — plus plans to identify safe sites for temporary shelters and finalise the post-disaster needs assessment report (ePardafas, 1 October 2026). Chaired by Home Minister Sudhan Gurung at the Home Ministry, the same 37th meeting heard that 1,454 bodies and human remains had been retrieved, 112 identified and 1,292 managed through burial; 3,685 DNA samples were under testing (1,957 at the Nepal Police Central Forensic Laboratory and 1,728 at the National Forensic Laboratory) with international expert support, searches were continuing at two tunnel sites, and 278 families from seven local units had requested immediate temporary shelter (Radio Nepal, 30 September 2026). Ahead of Dashain (11–21 October), the monsoon began withdrawing from Sudurpaschim, Karnali, western Lumbini and parts of western Gandaki on 5 October and is expected to leave Nepal entirely by about 10 October, with forecasters seeing no significant new weather systems during the core festival days (Meteorological Forecasting Division via The Kathmandu Post, 4 October 2026). Relief group Direct Relief said that as of 2 October it had shipped 21.5 tonnes of medical supplies and given US$125,000 in emergency grants to Mountain Heart Nepal, Shanti Foundation and One Heart Worldwide (Direct Relief, 2 October 2026). On 5 October 2026, about 40 days after the flood, the National Council for Disaster Risk Reduction and Management chaired by Prime Minister Balendra Shah suspended the Bhotekoshi–Trishuli search-and-rescue phase except for urgent operations and recommended Rs 559.17 billion to the finance ministry for 504 reconstruction and rehabilitation plans (The Kathmandu Post; OnlineKhabar, 5 October 2026). NDRRMA figures reported the same day put Nepal’s toll at 1,455 dead and 5,285 missing, and the rapid disaster needs assessment estimates NPR 408.28 billion in damage and losses and NPR 723 billion in reconstruction needs (IANS, 5 October 2026). The Ministry of Physical Infrastructure Development also said it is setting up a Maintenance and Disaster Resilience Unit and revising road and bridge design codes, because floods now carry far more sediment and debris; some crossings may need taller, longer bridges (Joint Secretary Bhimarjun Adhikari via OnlineKhabar, 5 October 2026). Despite the monsoon’s withdrawal, meteorologist Dr Binod Pokharel said on 5 October that rain would increase across Nepal through 8 October, with widespread rain on Wednesday 7 October and possible heavy falls in Sudurpaschim, easing only around Ghatasthapana, the first day of Dashain (OnlineKhabar, 5 October 2026). On 6 October the World Bank’s Nepal Development Update said the Rasuwa floods would cut Nepal’s growth this fiscal year to 3.7%, with a recovery to 5.2% projected for 2027/28, citing damage to hydropower, transmission and transport. The same day, the Home and Law ministries told a parliamentary special committee that the Disaster Risk Reduction and Management Act and the National Identity Card and Registration Act will be amended, on a fast track if needed, so that missing people can be registered as dead and their families can claim relief. Officials put the number of bodies recovered at 1,457 (OnlineKhabar, 6 October 2026). The disaster still has no official name: a seven-member expert committee formed by the Ministry of Energy, Water Resources and Irrigation on 18 September and led by water policy expert Devesh Belbase is weighing options such as “2026 Langtang Ice Rock Avalanche” and “glacial flood”, has two months to report, and no Nepali government team has yet reached the Lhende source area; “Himalayan tsunami”, the term Prime Minister Balendra Shah used at the UN General Assembly on 25 September, is not on its list (Kathmandu Post, 6 October 2026). Separately, Agriculture, Forests and Environment Minister Gita Chaudhary and visiting WWF-US and WWF Nepal delegations agreed to cooperate on post-disaster reconstruction and climate resilience; no funding amount was announced (OnlineKhabar, 6 October 2026). Physical Infrastructure Minister Sunil Lamsal told the parliamentary special committee on 6 October that Rasuwa flood survivors would be resettled before Dashain; officials said 12 of 20 damaged suspension bridges have been repaired, 8 are under repair, and four to five Bailey bridges are still needed for full road connectivity (Ratopati, 6 October 2026). A 55-member Nepali Army team is installing a 74-metre, 60-tonne Bailey bridge at Phalakhu Khola, Betrawati, to relink Nuwakot and Rasuwa, with completion targeted before Phulpati (Ratopati, 5 October 2026). On 7 October the parliamentary special committee studying the Trishuli–Bhotekoshi disaster, chaired by Ganesh Parajuli, met federal, provincial and local officials at Bidur, Nuwakot, on search, relief and temporary shelter; local representatives asked for immediate legal amendments to restore basic services and communications (Ratopati, 7 October 2026). FNCCI president Anjan Shrestha told the committee (6 October) that 85% of affected businesses in the Trishuli corridor are small and medium enterprises and asked for a relief-and-bailout package and a separate private-sector damage assessment (Ratopati, 6 October 2026). On 7 October the Cabinet recommended that President Ram Chandra Paudel issue an ordinance amending disaster-related laws so that people missing after a disaster can be declared dead after about 45 days instead of the current 12 years; government spokesperson Sasmit Pokharel called the change “quite significant” (OnlineKhabar, 7 October 2026). Physical Infrastructure Secretary Padam Kumar Mainali said reaching Rasuwagadhi will take “a few more months”: about 40 km of road was washed out, including the 16 km Syabrubesi–Timure–Rasuwagadhi stretch, with main-road damage put at about NPR 20 billion and motorable-bridge damage at NPR 13.8 billion (Ratopati, 7 October 2026). As of 8pm on 7 October, the Prime Minister’s relief fund accounts held about Rs 17.07 billion (up from about Rs 12.43 billion in mid-September), of which Rs 1 billion has been disbursed to flood-affected areas, per the Office of the Prime Minister and Council of Ministers (Ratopati, 7 October 2026). Road project chief Krishnanath Ojha said the Bailey bridge over the Phalakhu (Falakhu) river would be installed “within five days at most,” after which work would start on the Syabrubesi side; the Rasuwagadhi border crossing remains shut (The Kathmandu Post, 7 October 2026). After displaced Bidur and Tupche residents reported still receiving electricity bills with penalties and VAT for destroyed homes, Nepal Electricity Authority spokesperson Rajan Dhakal said the utility had decided to stop billing affected customers (The Kathmandu Post, 8 October 2026). On 8 October the National Disaster Risk Reduction and Management Authority began preparing temporary housing, asking NGOs to submit how many homes they will build and where; an initial 400–500 families need two-room homes of about 320 sq ft, costed at Rs 200,000–500,000 each, with 17 holding centres still sheltering 1,085 people in Nuwakot, Rasuwa and Dhading (OnlineKhabar, 8 October 2026). The same day, a Bagmati provincial assessment handed to Chief Minister Kiran Thapa Magar put damage to roads, bridges and government buildings at Rs 5.69 billion and to businesses at over Rs 2.97 billion; the province will give Rs 25 million in grants to 12 local units and seek a further Rs 1 billion from the federal government (The Kathmandu Post, 8 October 2026). Uphill, the flood never reached Gatlang in Aamachhodingmo Rural Municipality, but the loss of the Betrawati bridge has left it cut off from markets more than a month on: about 400 households farm vegetables commercially, ward 3 alone sold about Rs 30 million worth last year, and a request to fly produce out on the World Food Programme helicopter was not possible, leaving crops at risk of rotting before Dashain (The Kathmandu Post, 7 October 2026). The Cabinet’s three ordinances — including the disaster-management amendment cutting the wait to declare missing people dead from 12 years to 45 days — reached the President’s Office at about 5pm on 8 October but had not yet been formally presented to President Ram Chandra Paudel, and take effect only once he issues them (President’s Office spokesperson Krishna Bahadur Shahi via OnlineKhabar, 8 October 2026). Also on 8 October, Japanese Ambassador Maeda Toru handed DNA testing equipment and reagents to the Nepal Police Central Forensic Science Lab as emergency relief to help identify flood victims; no value was disclosed (Nepal News, 8 October 2026). On 9 October President Paudel issued the disaster ordinance (Ordinance to Amend Certain Nepal Acts Relating to Disasters, 2026), so the 45-day rule is now in force; the land and forest ordinances are still under study (Shahi via OnlineKhabar, 9 October 2026). The Home Ministry also gazetted flood- and landslide-hit areas of Gorkha, Manang, Myagdi, Baglung, Parbat and Nawalparasi (West) — hit between Asoj 8 and 11 (late September) — as disaster-hit areas for three months, a step meant to ease delivery of international relief (OnlineKhabar, 9 October 2026). A 45-day government stock-take published on 9 October put the preliminary count of affected people at 32,936 and displaced households at 8,317; families outside holding centres receive Rs15,000 a month in rent support for up to six months, and about Rs130 million (Rs13 crore) has gone from the Prime Minister’s relief fund to 14 local governments. About 450 MW of hydropower went offline, roughly 300 MW of it fully damaged, and NEA spokesperson Rajan Dhakal said about 150 MW from undamaged plants would be routed via Chilime directly to Matatirtha substation in Kathmandu (Ratopati, 9 October 2026). The Department of Urban Development and Building Construction said on 9 October that it would build 50 temporary prefabricated houses for Bhotekoshi flood victims on about 100 ropanis of land in Bidur Municipality, Nuwakot, for handover before Phulpati, at about Rs600,000 each (roughly Rs30 million) from the Prime Minister’s relief fund; Director General Dilip Bhandari put the eventual need at about 600 houses, down from an earlier estimate of 1,200 (Republica, 9 October 2026). As the 45-day mark passed on 10 October, ground searches for nine South Korean workers missing at the Upper Trishuli-1 hydropower site (three from Korea South-East Power, six from Doosan Enerbility) were expected to wind down ahead of Dashain, except for heavy-equipment excavation (Seoul Economic Daily, 10 October 2026).

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⚠️ How we classify these disasters. Not every Himalayan flood is a glacial lake outburst flood (GLOF). Some are rock–ice avalanches, some are landslide-dammed floods, most are cascades that change type as they move downhill. Each event on this page is labelled by its best available post-event science: GLOF, ice–rock avalanche, river-blockage flood or debris flow. If research revises a classification — as it did for Chamoli — we update the entry rather than keep the original headline.

🧠 The 60-second answer

On 26 August 2026, a large section of the Langtang Lirung glacier and surrounding rock broke off at about 5,200 m elevation on the Tibetan side of the Nepal–China border and fell roughly 1,200 m into the Lhende Khola valley. The resulting ice–rock avalanche briefly dammed the river; when the natural dam failed, a flood surged down the Bhote Koshi and Trishuli, raising the Trishuli by about 9 m in 30 minutes. The US Geological Survey first logged a magnitude-4.4 earthquake, then revised its analysis: no earthquake occurred — the magnitude-5.2 seismic signal was generated by the collapse itself. As of 5 October 2026, Nepal’s National Disaster Risk Reduction and Management Authority put the toll at 1,455 dead and 5,285 missing in Nepal alone — down from 5,786 missing on 21 September and 6,145 on 18 September as identification work reclassified some of the unaccounted — plus a further 43 dead and 519 missing in Tibet (as of 6 September) — making it by far the deadliest of the five events on this page. A second barrier lake that formed downstream after the collapse drained without a major breach by 30 August. It is the fifth major Himalayan glacier disaster since 2021, after Chamoli (2021), South Lhonak/Sikkim (2023), Thame (2024) and Rasuwa (2025) — and the same river corridor flooded from a glacial source just 13 months earlier.

🚨 Nepal–Tibet Glacier Disaster — Latest Verified Status
26 Aug 2026
Collapse date (~08:40 local)
~1,200 m
Vertical fall (~3,900 ft)
M5.2
Seismic signal (landslide, not quake)
~9 m
Trishuli rise in ~30 min
~1,498
Dead (1,455 Nepal / 43 Tibet)
~5,804
Missing (~5,285 Nepal / 519 Tibet)
~897
Foreign nationals missing (636 Nepal / 261 Tibet)
37
Motorable bridges destroyed; ~55 km road lost
Last updated 23 September 2026 · Location: Lhende Khola → Bhote Koshi → Trishuli, Nepal–Tibet border (Rasuwagadhi corridor) · Sources: USGS, ICIMOD, NDRRMA / Prime Minister’s Secretariat RDNA via Kathmandu Post and IANS (8–10 Sep 2026), NDRRMA via Qazinform (21 Sep 2026), Kathmandu Post (19–23 Sep 2026), ADB Asian Development Outlook (23 Sep 2026), UN Secretary-General UNGA address (22 Sep 2026), Chinese state media (6 Sep 2026), Reuters, AP, Al Jazeera. Casualty figures reflect the latest official update and may still be revised.
Status: source confirmed, toll still being reconciled. The collapsed glacier has been identified as Langtang Lirung. A second barrier lake that formed downstream drained without a major breach by 30 August 2026. A Nepal post-disaster review (Kathmandu Post, 2 September 2026) found the first public SMS alert went out roughly 38 minutes after the glacier collapse, to more than 600,000 phones downstream — too late for communities closest to the flood’s path — and the Syabrubesi hydrological station stopped transmitting data shortly after the flooding began, cutting off a key real-time source. A separate preliminary UNDP estimate (1 September 2026) put debris left along the Bhote Koshi–Trishuli corridor at roughly 2.2 million tonnes. Nepal’s National Disaster Risk Reduction and Management Authority put preliminary economic losses from the disaster at roughly Rs 387.54 billion as of 3 September 2026, with early government and expert assessments suggesting a reconstruction bill of Rs 800–900 billion. The Government of Nepal reported roughly 13,098 people rescued (incl. more than 300 foreign nationals) as of 5 September 2026, and search teams kept finding survivors in flooded hydropower tunnels along the Trishuli into early September — including two workers pulled out alive nine days after the flood on 3 September 2026, and two more people, among them a Chinese worker, recovered alive from a tunnel and a buried house on 4–5 September 2026. Casualty figures below reflect Nepal Police’s situation update of 7 September 2026, with Tibet figures as of 6 September 2026, and may still be revised as search and recovery continue. A later Kathmandu Post update (8–9 September 2026, citing NDRRMA) raised Nepal’s toll to 1,377 dead, 5,326 missing and 6,827 injured. A government panel led by National Planning Commission vice-chair Gunakhar Bhatta began a six-week post-disaster needs assessment across seven sectors in early September 2026, alongside NDRRMA’s preliminary loss estimate of roughly Rs 400 billion; on 10 September 2026 the Prime Minister’s Secretariat released a joint NPC–NDRRMA Rapid Damage and Needs Assessment putting total reconstruction and recovery needs at Rs 723.315 billion (about US$4.74 billion), with a fuller Post-Disaster Needs Assessment and a donor conference still to come. By 11 September 2026 the missing count had been revised down to about 5,130, with 1,377 confirmed dead. More than 21,000 security personnel — including Nepali Army, Nepal Police and Armed Police Force units — remained deployed in the affected districts as of 7 September 2026. Nepal observed a national day of mourning on 7 September 2026 — the 13th day since the collapse, marking the end of the traditional Hindu mourning period — with flags flown at half-mast at government offices and Nepali missions abroad; families of the missing gathered near the Prime Minister’s Office and key ministries the same day to demand faster search and rescue efforts.
❄️ Himalayan Glacier Disaster — Quick Facts
RegionHindu Kush Himalaya — glaciers feeding 10 major Asian river basins
Ice-loss rate (ICIMOD, Mar 2026)Doubled since 2000; up to ~27 m thickness lost since 1975
GLOF record (High Mountain Asia)700+ documented outburst floods over ~two centuries
Deadliest recent GLOFSouth Lhonak, Sikkim, Oct 2023 — ~50 million m³ released
Largest recent ice–rock avalancheChamoli, Feb 2021 — ~27 million m³ of rock and ice
People downstream in the HKH basinsWater resources important to nearly 2 billion (ICIMOD)
⚡ Quick Answers — AI Overview Ready

Himalayan glacier disasters: key questions

What caused the Nepal–Tibet flood in August 2026?
A large glacier-and-rock collapse on the Tibetan side of the border fell about 1,200 m, became an ice–rock avalanche, temporarily blocked the Lhende Khola, and then released a flood that swept down the Bhote Koshi and Trishuli. It was not a classic glacial lake outburst.
Was the 2026 Nepal flood caused by an earthquake?
Current evidence says no. The USGS first reported a magnitude-4.4 earthquake, then revised its assessment: no tectonic earthquake occurred, and the magnitude-5.2 seismic signal was generated by the collapsing mass of ice and rock itself.
What is the difference between a GLOF and an ice–rock avalanche?
A GLOF is a sudden release of water stored in or beside a glacier, usually when a moraine or ice barrier fails. An ice–rock avalanche is a mass of rock and glacier ice detaching from a steep slope. Both can cause downstream floods, sometimes in sequence.
Are Himalayan glaciers melting faster?
Yes. ICIMOD reported in March 2026 that ice-loss rates across the Hindu Kush Himalaya have doubled since 2000, with a marked acceleration after 2010. This is a regional aggregate, not an identical rate for every glacier.
📚 Key Takeaways

What connects five very different disasters

  • No single trigger. Chamoli 2021 was a rock–ice avalanche; Sikkim 2023 was a true GLOF; Thame 2024 was a lake failure that cascaded through two lakes; Rasuwa 2025 was a supraglacial-lake drainage; Nepal–Tibet 2026 was a glacier collapse that dammed a river.
  • The cascade is the danger. Each event changed form as it travelled — avalanche to debris flow, mass movement to displacement wave to dam breach. The kill mechanism was rarely the initiating one.
  • 2026 was not a classic GLOF. Do not file it with Sikkim or Thame. The primary trigger was a glacier/rock collapse; the flood came from a temporary river blockage failing.
  • The earthquake report was wrong. The USGS revised its own analysis — the seismic signal came from the landslide, not a fault rupture.
  • The warning system was not built for this. Nepal’s post-disaster review (Kathmandu Post, 2 Sept 2026) found the first public alert went out ~38 minutes after the collapse, after a key hydrological station stopped transmitting — too late for the nearest communities.
  • This valley had a recent warning. The July 2025 Rasuwa flood came down the same Lhende–Trishuli corridor from a glacial lake on the Tibetan side, destroying the Nepal–China Friendship Bridge.
  • Climate raises the background risk, not every single rock. Warming drives glacier retreat, permafrost thaw and lake growth — but attributing one slope collapse to climate change needs a dedicated study.
  • South Lhonak is the strongest climate link. Peer-reviewed work found climate-driven glacier retreat and permafrost degradation amplified the 2023 hazard.
  • Ice loss has doubled. ICIMOD (March 2026): Hindu Kush Himalaya glacier ice-loss rates roughly doubled since 2000; up to ~27 m of thickness gone since 1975.
  • Hydropower sits in the blast zone. Rishiganga, Tapovan, Teesta III and Rasuwagadhi were all damaged or destroyed — the same steep valleys that generate power carry the floods.
  • Collapses are hard to forecast. Monitoring can flag a growing lake or a creeping slope; it cannot reliably predict the day a glacier lets go.

What caused the 2026 Nepal–Tibet disaster?

The sequence, step by step — from a current, still-preliminary reconstruction.

A glacier and rock collapse became an ice–rock avalanche, which blocked a river and then released a flood. At about 08:40 local time on 26 August 2026, satellite imagery indicates a substantial section of the lower end of the Langtang Lirung glacier detached at roughly 5,200 m on the Tibetan side of the border and fell about 1,200 m onto the valley floor, entraining rock and sediment as it went. The avalanche struck the Lhende Khola about 20 km northeast of the Rasuwagadhi border crossing.

What happened next is what made it a transboundary catastrophe:

  1. The debris temporarily blocked the Lhende Khola, ponding water behind an unstable natural dam.
  2. The blockage failed — landslide and avalanche dams often fail within hours — releasing the ponded water in a surge.
  3. The surge picked up sediment and became a debris-laden flood moving down the Bhote Koshi.
  4. Downstream on the Trishuli, water levels rose by as much as nine metres in about half an hour, according to river monitoring reported by ICIMOD and news agencies.
  5. The flood destroyed 37 motorable bridges and damaged dozens more suspension bridges, washed away roughly 55 km of road, damaged hydropower facilities and hit the Rasuwagadhi border area.

Note what this was not. It was not a magnitude-5.2 earthquake. It was not friction “melting the glacier into a flood.” It was not, on current evidence, a classic glacial lake outburst — there is no confirmed lake as the primary trigger. It was a high-mobility mass movement that interacted with a river. Measurements still being verified include the exact detached area (early estimates put the collapsed slab at roughly 600 m wide) and the precise contribution of recent high temperatures; the source glacier has since been identified as Langtang Lirung.

Was the Nepal–Tibet flood triggered by an earthquake?

Current evidence says no. The event was initially interpreted as an earthquake — the USGS logged a magnitude-4.4 event about 66 km north of Kathmandu — but the USGS later determined that no earthquake had occurred. Using data from nearby seismic stations, long-period seismic waves and satellite imagery, it concluded that the seismic signal was generated by the glacier and rock collapse itself, and reclassified it as a magnitude-5.2 landslide.

Can a landslide really produce a magnitude-5.2 signal?

Yes. Seismic magnitude measures the strength of recorded ground motion, whatever its source. A large, fast mass movement — a rock avalanche, a glacier collapse — shakes the ground and radiates seismic waves that instruments record and can assign a magnitude to. For comparison, the 2022 Marmolada glacier collapse in the Italian Dolomites registered around magnitude 0.6.

So “a magnitude-5.2 seismic event” is accurate; “a magnitude-5.2 tectonic earthquake” is not. The distinction matters because an earthquake-triggered collapse and a spontaneous collapse imply very different monitoring and warning strategies.

How a warming mountain can become a flash flood

One possible cascading pathway — not every Himalayan flood follows this sequence.

Warming — rising air and ground temperatures in the high mountains
▼
Glacier retreat + permafrost thaw — ice thins, slopes lose support, ice in rock fractures melts
▼
Slope instability — fractured rock and hanging ice become more vulnerable to failure
▼
Ice–rock avalanche — a mass detaches, accelerates, fragments and entrains snow, sediment and water
▼
River impact / temporary blockage — the flow reaches a valley river and dams it, or enters a glacial lake and displaces water
▼
Natural dam failure or wave overtopping — ponded or displaced water is released suddenly
▼
Flash flood / debris flow — a sediment-rich surge moves tens to hundreds of kilometres downstream
▼
Impact — bridges, roads, hydropower, farmland and communities in the valley

Warming does not mechanically cause each individual avalanche. It changes the conditions that make failures more likely and lakes larger.

GLOF vs ice–rock avalanche: they are not the same disaster

FeatureGlacial lake outburst flood (GLOF)Ice / rock avalanche
Initial triggerSudden release of water from a glacial lake (barrier fails, or a mass movement enters the lake)A rock-and-ice mass detaches from a steep slope or glacier
Main moving materialWater plus sediment and debrisIce, rock, snow and sediment
Can block a river?Sometimes, via the debris it carriesYes — directly
Can cause a downstream flood?Yes — that is the defining outcomeYes — directly, or after damming a river
Needs a lake?Yes, by definitionNo
Clear Himalayan exampleSouth Lhonak, Sikkim (2023); Thame (2024)Chamoli (2021)
2026 Nepal–TibetNot classified as a classic GLOF on current evidenceGlacier / rock collapse → river blockage → debris flood

2026 in one line, against the others

2023 Sikkim: GLOF.   2021 Chamoli: rock–ice avalanche.   2024 Thame: GLOF (two-lake cascade).   2025 Rasuwa: supraglacial-lake outburst.   2026 Nepal–Tibet: ice–rock / glacier collapse → river-blockage flood.

The five events at a glance

Ranked by released water volume or collapsed mass, where measured. Every figure is from post-event science.

1
~50Mm³ water released
South Lhonak, Sikkim
3–4 October 2023 · GLOF
TriggerLateral moraine collapse into lake (up to 14.7M m³)
Wave~20 m displacement wave breached the dam
Key lossTeesta III (1,200 MW) dam destroyed

India

2
~27Mm³ rock + ice
Chamoli (Ronti Peak)
7 February 2021 · Rock–ice avalanche
SourceSteep north face of Ronti Peak, ~5,500 m
RunoutScoured valley walls up to 220 m above the bed
Key lossRishiganga + Tapovan hydropower; 200+ dead

India (Uttarakhand)

3
~1,200m vertical fall
Nepal–Tibet border
26 August 2026 · Glacier / rock collapse
MechanismAvalanche → river blockage → dam-break flood
SurgeTrishuli +9 m in ~30 min
Toll (5 Oct 2026)~1,498 dead, ~5,804 missing

Nepal + Tibet/China

4
~0.46Mm³ released (two lakes)
Thame, Khumbu
16 August 2024 · GLOF cascade
TriggerRock avalanche into a lake at 4,900 m → wave → two dam breaches
Damage14 buildings incl. school & health post; ~135 people hit
NoteThyanbo lake was not on the “dangerous lakes” list

Nepal (Solukhumbu)

Himalayan glacier disaster timeline: 2021–2026

Newest first. Only scientifically distinct events, plus the data that frames them.

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26 AUG
2026

Nepal–Tibet: a glacier collapse becomes a transboundary catastrophe

Lhende Khola → Bhote Koshi → TrishuliIce–rock / glacier collapseStatus: preliminary

At about 08:40 local time, a substantial section of the lower end of the Langtang Lirung glacier detached at roughly 5,200 m on the Tibetan side of the border and fell about 1,200 m, gathering rock and sediment. The avalanche hit the Lhende Khola ~20 km northeast of the Rasuwagadhi crossing and temporarily blocked the river.

When the natural dam failed, a debris-laden flood surged down the Bhote Koshi and Trishuli. The Trishuli rose about 9 m in 30 minutes. The USGS first reported a magnitude-4.4 earthquake, then concluded no earthquake occurred and the magnitude-5.2 signal was produced by the collapse.

As of 5 Sep 2026 (Government of Nepal situation update): 1,344 bodies recovered and about 5,000 missing in Nepal, plus 43 dead and 519 missing in Tibet’s Gyirong County (incl. ~261 foreign nationals), as of 6 Sep 2026. A Rapid Damage and Needs Assessment counted 37 motorable bridges destroyed, 68 suspension bridges damaged, about 55 km of roads damaged and roughly 783 MW of hydropower capacity lost across 13 affected projects. The government reported roughly 13,098 people rescued overall (incl. more than 300 foreign nationals) as of 5 September 2026, and survivors kept being found in flooded hydropower tunnels along the Trishuli into early September, including two workers pulled out alive nine days after the flood on 3 September 2026 and two more people recovered alive on 4–5 September. UNDP’s 1 September 2026 preliminary estimate put debris along the Bhote Koshi–Trishuli corridor at roughly 2.2 million tonnes. A second barrier lake downstream drained safely by 30 August.
ICE–ROCK AVALANCHERIVER BLOCKAGEUNDER INVESTIGATION

ICIMOD: Hindu Kush Himalaya ice-loss rates have doubled since 2000

HKH Glacier Outlook 2026Regional aggregate

On 21 March 2026, ICIMOD published its HKH Glacier Outlook 2026, synthesising 38 monitored glaciers. Headline finding: ice-loss rates roughly doubled since 2000, with a marked acceleration after 2010, strongest in the eastern and central Himalaya. The reports also cite up to ~27 m of ice-thickness loss since 1975 and roughly a 12% loss of glacier area between 1990 and 2020.

This is a different metric from ICIMOD’s 2023 assessment, which found HKH glaciers lost mass about 65% faster in 2011–2020 than in the previous decade. Related, but not the same statistic — do not merge them.
SCIENTIFIC ASSESSMENT~2 BILLION DOWNSTREAM
8 JUL
2025

Rasuwa: a transboundary glacial flood hits the same corridor

Lhende River → Upper TrishuliSupraglacial-lake outburst

Early on 8 July 2025, a flood wave surged down the Lhende River in Tibet, crossed the border at Rasuwagadhi and entered Nepal’s Upper Trishuli. ICIMOD satellite analysis attributed it to the rapid growth and sudden drainage of a supraglacial lake on the Purepu Glacier in China’s Gyirong County, about 35 km upstream at ~5,150 m. The lake had grown to about 638,000 m² by 7 July and shrank sharply after the rupture.

At least 9 dead and 19 missing. The flood destroyed the Nepal–China Friendship Bridge, damaged the Rasuwagadhi hydropower project and border facilities, and caused losses reported in the billions of rupees up to ~100 km downstream.
GLOF (SUPRAGLACIAL)TRANSBOUNDARYPRIOR WARNING FOR 2026
16 AUG
2024

Thame: a glacial lake outburst above an Everest-region village

Thame valley, SolukhumbuGLOF — two-lake cascade

ICIMOD determined that the flood began when a rock avalanche hit a glacial lake at about 4,900 m, generating a displacement wave that breached the lake and released roughly 156,000 m³ of water. That outflow fell about 120 m, hit a second lake, and breached its moraine dam — leaving a gap about 22 m high and 51 m wide and releasing a further ~303,000 m³.

14 properties destroyed — 7 homes, 5 hotels, 1 school, 1 health post — and about 135 people affected in Thame. The Thyanbo lake system was not even listed among Nepal’s potentially dangerous glacial lakes.
GLOFCASCADENO FATALITIES REPORTED
3 OCT
2023

South Lhonak, Sikkim: a true glacial lake outburst flood

Teesta basin, SikkimGLOFPeer-reviewed

On the night of 3–4 October 2023, the moraine-dammed South Lhonak Lake released a catastrophic flood. Later research (published in Landslides, summarised by ICIMOD in 2025) found that an unstable lateral moraine mass — up to 14.7 million m³ of frozen material — collapsed into the lake, generating a roughly 20 m tsunami-like wave that eroded and breached the frontal moraine and released about 50 million m³ of water.

The unstable moraine section had been creeping at more than 15 m per year between 2016 and 2023. Permafrost was present in the failure zone, and thaw is thought to have contributed to the instability.

Downstream: Teesta III (1,200 MW) dam destroyed, plus bridges, roads and settlements along the Teesta. Casualty accounting varies by method — the peer-reviewed study lists about 55 confirmed dead and around 70 missing; earlier official and media totals ran to roughly 100 dead.
GLOFMORAINE COLLAPSESTRONG CLIMATE LINK
7 FEB
2021

Chamoli: the disaster first mistaken for a GLOF

Ronti Gad → Rishiganga → DhauligangaRock–ice avalancheUttarakhand

A wedge of rock and glacier ice — about 27 million m³ — detached from the steep north face of Ronti Peak, transformed into an extraordinarily mobile debris flow, and raced down the Ronti Gad, Rishiganga and Dhauliganga valleys. It carried boulders more than 20 m across and scoured valley walls up to 220 m above the river bed.

Early reports called it a glacial lake outburst flood. A 2021 study in Science established a rock-and-ice avalanche origin with no lake involved — the clearest example of why mechanism must be checked, not assumed.

More than 200 people were killed; of 204 dead or missing, about 190 were workers at the Rishiganga (13.2 MW) and Tapovan (520 MW) hydropower projects, both under construction. Later analyses point to precursory signs such as fracturing and slope deformation before the collapse.
ROCK–ICE AVALANCHENOT A GLOFHYDROPOWER LOSS
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Nepal–Tibet flood casualty tracker

A snapshot, not a running total. Figures from different update times must not be added together.

AreaConfirmed deadMissingAs ofSource basis
Nepal1,4555,2855 Oct 2026Nepal’s NDRRMA (via IANS)
Tibet / China (Gyirong County)43519 (incl. ~261 foreign nationals)6 Sep 2026Chinese state media
Reported total~1,498~5,8045 Oct (Nepal) / 6 Sep 2026 (Tibet)Combined agency reporting

Why the numbers keep changing

In a debris flood, “missing” and “confirmed dead” move as bodies are recovered, as people are found alive in cut-off villages, and as tourist and worker registers are reconciled across two countries. Reported missing foreign trekkers in Nepal come from more than 20 countries; the largest groups named so far are Indian, US, Australian, British and Canadian nationals. Authorities have not released names. Expect these figures to be revised.

Disaster comparison table

Update as scientific investigations evolve.

EventInitial triggerLake involved?Main flood mechanismMajor infrastructure impact
Chamoli 2021Rock / ice avalanche (Ronti Peak)NoAvalanche → mobile debris flowRishiganga & Tapovan hydropower
South Lhonak 2023Lateral moraine mass into the lakeYesDisplacement wave → dam breach (GLOF)Teesta III dam; Teesta-valley bridges/roads
Thame 2024Rock avalanche into a glacial lakeYes (two lakes)Wave → breach → second breach (GLOF cascade)Village buildings, school, health post
Rasuwa 2025Supraglacial-lake growth & drainage (Purepu Glacier)Yes (supraglacial)Sudden lake drainage → transboundary floodFriendship Bridge; Rasuwagadhi hydropower
Nepal–Tibet 2026Glacier / rock collapseNot the primary triggerAvalanche → river blockage → dam-break flood37 motorable + 68 suspension bridges; ~55 km road; ~783 MW hydropower

Did climate change cause the 2026 Nepal–Tibet disaster?

Climate change cannot be assigned as the sole cause of a single slope collapse before attribution and geomorphological studies are done. Scientists studying the 2026 event say it is too early to quantify how much warming contributed, though several have pointed to rapid melt and high temperatures as plausible contributing factors.

What warming clearly does is raise the background conditions associated with high-mountain instability:

  • Glacier retreat exposes and de-buttresses steep valley walls that ice used to support.
  • Permafrost thaw melts the ice that helps bind fractured rock masses together.
  • Altered meltwater can push water into rock fractures and lubricate slip surfaces.
  • Expanding glacial lakes store more water behind moraine dams that were never engineered.
  • Changing snow and ice conditions shift where and when avalanches start.

The honest phrasing is contributed to the risk, not proved the sole cause — unless a specific study establishes otherwise.

Climate attribution, event by event
EventAttribution statusWhat the evidence shows
South Lhonak 2023Strong published evidencePeer-reviewed work found climate-driven glacier retreat and permafrost degradation amplified the hazard
Thame 2024Emerging evidenceICIMOD frames it as part of accelerating cryosphere hazards in the Everest region; formal attribution limited
Chamoli 2021Possible contributing factorStudies note warming and development raise Himalayan risk; the collapse itself was not formally attributed
Rasuwa 2025Possible contributing factorSupraglacial lake formed and grew rapidly in a warming, fast-melting basin
Nepal–Tibet 2026Not yet attributedInvestigation ongoing; rapid melt and high temperatures flagged as suspected contributors

Himalayan glacier loss has accelerated

What ICIMOD reported (Mar 2026)

  • Ice-loss rates across the Hindu Kush Himalaya have roughly doubled since 2000
  • Loss accelerated after 2010, strongest in the eastern and central Himalaya, hitting smaller glaciers hardest
  • Up to ~27 m of ice-thickness loss since 1975 across monitored glacier datasets
  • The region lost roughly 12% of its glacier area between 1990 and 2020
  • Synthesis of 38 monitored glaciers; water resources important to nearly 2 billion people downstream

What it does not mean

  • Not “every Himalayan glacier melts twice as fast” — this is a regional aggregate
  • Not the same as the 2023 ICIMOD figure (65% faster mass loss in 2011–2020 vs the prior decade) — different metric and timeframe
  • Not “2 billion people will lose their water” — basin hydrology is far more complex
  • Not a prediction that a specific lake or slope will fail on a specific date
  • Ice-thickness loss is not the same as area loss or mass-balance rate — keep the metrics separate

Why Himalayan hydropower is exposed

Hydropower projects sit in steep river valleys because that is where the fall and the flow are. The same geography puts them directly in the path of floods, debris flows, landslides and GLOFs. The pattern repeats across every event on this page:

  • Chamoli 2021: the Rishiganga plant was destroyed and the larger Tapovan-Vishnugad project badly damaged; most of the dead were construction workers on site.
  • South Lhonak 2023: the 1,200 MW Teesta III dam was destroyed, worsening the downstream surge.
  • Rasuwa 2025 and Nepal–Tibet 2026: the Rasuwagadhi project and other Bhote Koshi / Trishuli plants were damaged, and border infrastructure was cut.

Damaged hydropower infrastructure can also amplify a cascade — a failed or overtopped structure adds water and sediment to the flood, and its loss compounds the economic damage. This does not mean hydropower caused the initiating glacier events; it means siting, design and early-warning integration matter enormously in these valleys. Figures sometimes quoted for regional “hydropower potential” (for example 500 GW) describe theoretical or technical potential across the wider region, not installed capacity — the two are very different.

Why rescue is so hard after a Himalayan debris flood

The same flood that causes the disaster also destroys the means of responding to it:

  • Roads and bridges are gone — in 2026, 37 motorable bridges were destroyed and about 55 km of road washed out, isolating whole valleys.
  • Sediment, not just water — debris floods leave metres of mud and boulders that bury vehicles, buildings and victims.
  • River levels stay high and unstable for days, and secondary landslides keep coming.
  • Terrain limits helicopters — narrow valleys, high altitude and few safe landing sites.
  • Weather and communications — monsoon cloud grounds aircraft; power and mobile networks fail.
  • Two countries — a transboundary event needs coordinated search, data-sharing and consular work across a closed border.

Can scientists predict a glacier collapse?

Not reliably in every case. Monitoring can detect slope movement, fractures, lake expansion, changes in glacier velocity, seismic signals and melt conditions — and researchers had flagged South Lhonak as a hazardous, rapidly growing lake years before it failed. But that is hazard identification, not a forecast of the failure date. Sudden collapses of ice and rock remain very difficult to predict precisely.

What a GLOF early-warning system looks like

Possible components include lake-level sensors, river gauges, weather stations, satellite monitoring, seismic monitoring, automated alerts and downstream sirens with evacuation routes. Nepal has installed such systems on some rivers. The limits are structural: remote headwaters, cross-border catchments where the trigger sits in another country, power and maintenance in the high mountains, and the need for people downstream to know what a siren means and where to run.

Satellites are now essential

Optical imagery, synthetic aperture radar (SAR) and InSAR let analysts map lake growth, measure slow slope deformation, and produce before-and-after images of a collapse scar and flood path within days. This is powerful for understanding an event and tracking building hazards — it is not yet real-time collapse detection.

What satellite data later showed about the 2026 collapse

A post-event analysis reported in Nature (September 2026) found that the ice-and-rock mass above Langtang Lirung had been creeping at roughly 10 mm per month between January and mid-August 2026, then accelerated in the weeks immediately before the 26 August collapse; imagery also showed diminishing snow cover and more exposed bare ice on the slope beforehand. The signal was real and visible in hindsight — but turning slow-creep satellite data into a real-time public warning, days or weeks ahead, remains unsolved.

A glacier can collapse in one country and flood another

The 2025 and 2026 disasters both began in Tibet and did their worst damage in Nepal. Headwaters in one jurisdiction and communities in another make preparedness a matter of data-sharing, joint river monitoring and cross-border warning protocols, not just national systems. If a 2026-style flood prompts alerts or evacuations further downstream in India, those should be reported from official Indian agencies (CWC, NDMA, state authorities) rather than assumed.

The science, defined

Plain definitions for the terms this story turns on.

Definition

Glacial lake outburst flood (GLOF)

The sudden release of water stored in or beside a glacier — often when a moraine or ice barrier fails, or when a mass movement enters the lake and pushes out a displacement wave. Triggers vary: avalanche, rockfall, moraine instability, ice collapse, heavy rain, lake-level rise or ice-dam melt. In High Mountain Asia, a large share of documented GLOFs were set off by mass movement into a lake.

Definition

Ice–rock avalanche

A large mass of rock and glacier ice that detaches from steep high-mountain terrain and accelerates downslope. It can fragment, entrain snow, sediment and water, travel long distances, enter rivers, and trigger secondary floods or debris flows. Chamoli 2021 is the clearest recent Himalayan example.

Definition

Debris flow (“liquid concrete”)

A fast, dense mixture of water, mud, sand, boulders, ice, wood and whatever infrastructure it destroys. The high sediment concentration is what gives it such destructive force. “Liquid concrete” is a useful description, not a scientific classification.

Definition

Permafrost

Ground that stays frozen for at least two consecutive years. In high mountains, ice inside rock fractures helps hold rock masses together. Warming can thaw that ice and contribute to instability — though thaw alone is rarely a confirmed sole trigger for any single collapse.

Definition

River-blockage (landslide-dam) flood

When an avalanche or landslide dumps enough material into a river to dam it, water ponds behind the blockage. These natural dams are unconsolidated and often fail within hours, releasing a sudden downstream flood. This is the mechanism behind the 2026 Nepal–Tibet surge.

Context

Hindu Kush Himalaya (HKH)

A high-mountain system spanning eight countries, far larger than “the Himalayas” alone. Its glaciers and snow feed ten major river basins — the Indus, Ganga, Brahmaputra, Mekong, Yangtze and more — which is why ICIMOD calls it the “Water Towers of Asia.”

High mountains in a warming world

The Himalayas are not alone — but the hazards differ by region.

RegionPrimary glacier-linked hazardRecent example
Himalayas / Hindu Kush HimalayaGLOFs and ice–rock avalanchesChamoli 2021; South Lhonak 2023; Nepal–Tibet 2026
European AlpsPermafrost thaw and rock / rock–ice instabilityMarmolada collapse 2022; Blatten (Switzerland) rock-avalanche and river dam 2025
AndesGlacial-lake growth and outburst riskLong history of Cordillera Blanca GLOFs (Peru)
AlaskaGlacier retreat, landslides and landslide-generated wavesDocumented tsunami hazard in rapidly deglaciating fjords
GreenlandLarge rock avalanches into fjords2023 Dickson Fjord landslide generated a days-long seiche

These regions do not face identical hazard intensity. The Himalayas stand out because so many people, roads, dams and trekking routes sit in the valleys directly downstream of unstable ice.

Disaster risk is more than the glacier

Hazard — the glacier, the slope, the lake and how likely each is to fail
✕
Exposure — the people, roads, bridges, dams, hotels and towns in the path
✕
Vulnerability — whether there is warning, whether construction can survive a surge, whether people can evacuate
=
Disaster risk

A glacier collapse in an empty valley may harm no one. The same collapse above a road, a dam, a trekking season and a border crossing becomes a catastrophe. Warming raises the hazard term; development raises the exposure term.

Myth vs reality

MythReality
Every Himalayan glacier disaster is a GLOF.Some are rock–ice avalanches, landslides or cascading river-blockage floods with no lake as the primary trigger.
The 2026 event was a magnitude-5.2 earthquake.The USGS concluded no earthquake occurred; the collapse itself generated the magnitude-5.2 seismic signal.
Glaciers simply melt and become floods.Mass movement, river blockage, sediment entrainment and lake failure all play roles. Friction does not just “melt the glacier into water.”
If a dangerous glacial lake is mapped, the disaster can be predicted.Hazard mapping improves preparedness but does not give an exact failure time. South Lhonak was studied for years before it failed.
Glacier collapses are becoming common.Warming is increasing several underlying hazards, but rare ice–rock collapses remain hard to quantify and predict.

Latest Himalayan glacier disaster updates

Updated only for meaningful scientific or rescue developments.

Update log

  • 11 October 2026: DUDBC to build 50 temporary prefabricated houses for Bhotekoshi flood victims on about 100 ropanis in Bidur, Nuwakot, before Phulpati (about Rs600,000 each, roughly Rs30 million, from the PM relief fund); eventual need put at about 600 houses, down from 1,200 (DG Dilip Bhandari via Republica, 9 October). Ground searches for nine South Korean workers missing at Upper Trishuli-1 expected to wind down ahead of Dashain (Seoul Economic Daily, 10 October). Toll unchanged at 1,455 dead and 5,285 missing (NDRRMA).
  • 10 October 2026: Government 45-day stock-take: 32,936 people affected and 8,317 households displaced (preliminary); Rs15,000 monthly rent support for up to six months for families outside holding centres; about Rs13 crore sent from the PM relief fund to 14 local governments; about 450 MW of hydropower offline, roughly 300 MW fully damaged, with about 150 MW from undamaged plants to be routed via Chilime to Matatirtha substation (NEA’s Rajan Dhakal via Ratopati, 9 October). Toll unchanged at 1,455 dead and 5,285 missing (NDRRMA).
  • 9 October 2026 (evening): President Paudel issued the disaster ordinance on 9 October, cutting the wait to declare disaster-missing people dead from 12 years to 45 days; land and forest ordinances still under review (OnlineKhabar, 9 October). Home Ministry gazette declared parts of Gorkha, Manang, Myagdi, Baglung, Parbat and Nawalparasi (West) disaster-hit areas for three months after late-September floods and landslides (OnlineKhabar, 9 October). Toll unchanged at 1,455 dead and 5,285 missing (NDRRMA).
  • 9 October 2026: Disaster-management ordinance (45-day rather than 12-year wait to declare missing people dead) and two others reached the President’s Office about 5pm on 8 October; not yet issued (OnlineKhabar, 8 October). Japan handed DNA testing equipment and reagents to the Nepal Police Central Forensic Science Lab to help identify victims, value not disclosed (Nepal News, 8 October). Toll unchanged at 1,455 dead and 5,285 missing (NDRRMA).
  • 8 October 2026 (night): Gatlang (Aamachhodingmo-3, Rasuwa) cut off from markets since the Betrawati bridge was swept away; about 400 households farm vegetables commercially, ward 3 sold about Rs 30 million last year, WFP helicopter request for produce not possible; NDRRMA says the 9.8 km Bidur–Betrawati stretch is cleared and the Dhunche–Betrawati road is in its final stage (The Kathmandu Post, 7 October). Toll unchanged at 1,455 dead and 5,285 missing.
  • 8 October 2026 (evening): NDRRMA began temporary-housing preparations, asking NGOs for build numbers, sites and timelines; initial need 400–500 families, two-room ~320 sq ft homes at Rs 200,000–500,000 each; 17 holding centres still house 1,085 people (OnlineKhabar, 8 October). Bagmati province assessment: Rs 5.69 billion damage to roads, bridges and public buildings, over Rs 2.97 billion to businesses; Rs 25 million in grants to 12 local units and a Rs 1 billion request to the federal government (The Kathmandu Post, 8 October). Toll unchanged at 1,455 dead and 5,285 missing.
  • 8 October 2026: Prime Minister’s relief fund accounts reached about Rs 17.07 billion as of 7 October evening, Rs 1 billion disbursed so far (Office of the Prime Minister via Ratopati, 7 October). Road project chief Krishnanath Ojha: Phalakhu Bailey bridge within five days, then work on the Syabrubesi side; Rasuwagadhi crossing still shut (The Kathmandu Post, 7 October). NEA spokesperson Rajan Dhakal said the utility will stop billing flood-affected customers whose homes were destroyed (The Kathmandu Post, 8 October). Toll unchanged at 1,455 dead and 5,285 missing (NDRRMA).
  • 7 October 2026 (night): Cabinet recommended a presidential ordinance amending disaster-related laws so missing people can be declared dead after about 45 days rather than 12 years, addressing Rasuwa flood families unable to obtain death certificates (spokesperson Sasmit Pokharel, OnlineKhabar, 7 October). Secretary Padam Kumar Mainali said the road to Rasuwagadhi needs “a few more months”; about 40 km washed out, including the entire 16 km Syabrubesi–Timure–Rasuwagadhi stretch; track to Syabrubesi expected after Dashain and Tihar (Ratopati, 7 October).
  • 7 October 2026 (evening): The parliamentary special committee on the Trishuli–Bhotekoshi disaster (chair Ganesh Parajuli) met officials from all three tiers of government in Bidur, Nuwakot, on search, relief and temporary shelter; local representatives sought immediate legal amendments to restore basic services and communications (Ratopati, 7 October). FNCCI president Anjan Shrestha asked the committee (6 October) for a relief-and-bailout package and a business revival plan, saying 85% of affected businesses are small and medium enterprises (Ratopati, 6 October). Toll unchanged at 1,455 dead / 5,285 missing (NDRRMA).
  • 7 October 2026: Minister Sunil Lamsal told the parliamentary special committee (6 October) that Rasuwa flood survivors will be resettled before Dashain; 12 of 20 damaged suspension bridges repaired, 8 under repair, four to five Bailey bridges still needed (Ratopati, 6 October). Nepali Army installing a 74-metre, 60-tonne Bailey bridge at Phalakhu Khola, Betrawati, targeted before Phulpati (Ratopati, 5 October). Toll unchanged at 1,455 dead / 5,285 missing (NDRRMA).
  • 6 October 2026 (late night): A ministry-appointed expert committee led by Devesh Belbase, formed 18 September with a two-month mandate, is still debating an official name for the 26 August disaster (options include “2026 Langtang Ice Rock Avalanche” and “glacial flood”); no Nepali government team has reached the Lhende source area (Kathmandu Post, 6 October). Nepal’s forest and environment ministry and WWF agreed to cooperate on post-disaster reconstruction and climate resilience, with no amount announced (OnlineKhabar, 6 October). Toll unchanged at 1,455 dead / 5,285 missing (NDRRMA).
  • 6 October 2026 (night): World Bank Nepal Development Update projects growth of 3.7% this fiscal year because of the Rasuwa floods, recovering to 5.2% in 2027/28 (OnlineKhabar, 6 October). The Home and Law ministries told a parliamentary special committee that two laws (the Disaster Risk Reduction and Management Act and the National Identity Card and Registration Act) will be amended so missing people can be registered as dead; officials cited 1,457 bodies recovered. NDRRMA tracker figure still 1,455 dead / 5,285 missing.
  • 6 October 2026 (evening): Forecasters say rain will increase nationwide through 8 October despite the monsoon’s withdrawal, with widespread rain on 7 October and possible heavy falls in Sudurpaschim, easing around Ghatasthapana (meteorologist Dr Binod Pokharel via OnlineKhabar, 5 October). Toll unchanged at 1,455 dead / 5,285 missing (NDRRMA).
  • 6 October 2026: Nepal’s Ministry of Physical Infrastructure Development says it is creating a Maintenance and Disaster Resilience Unit and revising road and bridge design codes for climate resilience after the Bhotekoshi–Trishuli and Kaligandaki floods; Road Department Director General Bijay Jaisi says basic road connectivity was restored within 15 days, including a temporary road at Krishnabhir designed in three days (OnlineKhabar, 5 October). Toll unchanged at 1,455 dead / 5,285 missing (NDRRMA).
  • 5 October 2026 (evening): The National Council for Disaster Risk Reduction and Management, chaired by Prime Minister Balendra Shah, suspends the Bhotekoshi–Trishuli search-and-rescue phase except for urgent operations and recommends Rs 559.17 billion to the finance ministry for 504 reconstruction and rehabilitation plans (The Kathmandu Post; OnlineKhabar, 5 October). NDRRMA puts Nepal’s toll at 1,455 dead and 5,285 missing; the rapid needs assessment estimates NPR 723 billion in reconstruction needs (IANS, 5 October). Tracker updated to 1,455 dead / 5,285 missing.
  • 5 October 2026: The monsoon began withdrawing from western Nepal on 5 October and is expected to exit the country by about 10 October, pointing to a drier Dashain (11–21 October) after weeks of flood and landslide disruption (Meteorological Forecasting Division via The Kathmandu Post, 4 October 2026). Direct Relief reported 21.5 tonnes of medical supplies shipped and US$125,000 in grants to three Nepali partners as of 2 October (Direct Relief).
  • 4 October 2026 (evening): Radio Nepal’s account of the 37th NDRRM Executive Committee meeting (chaired by Home Minister Sudhan Gurung) adds that 1,454 bodies and remains have been retrieved and 112 identified, 3,685 DNA samples are being tested at the Nepal Police Central Forensic Laboratory (1,957) and the National Forensic Laboratory (1,728), searches continue at two tunnel sites, and 278 families have sought temporary shelter; 5,285 remain missing (Radio Nepal, 30 September 2026).
  • 4 October 2026: The search-and-recovery shift was announced by NDRRMA executive chief Dharmaraj Upreti at Singha Durbar on 30 September, with missing persons to be certified by local governments, verified by District Administration Offices and then processed by NDRRMA; the authority also plans temporary shelters at safe sites and is finalising the post-disaster needs assessment (ePardafas, 1 October 2026).
  • 3 October 2026 (evening): The National Disaster Risk Reduction and Management Executive Committee’s 37th meeting shifted operations from search-and-rescue to search-and-recovery, keeping rescue only at critical, highly sensitive sites and prioritising recovery of bodies and damaged structures elsewhere; 5,285 remain missing. IPPAN secretary Bijay Mohan Bhattarai said about 1 km of road beyond Chilime must be rebuilt and access to some Rasuwa hydropower sites could take up to a year (OnlineKhabar, 3 October). Himlung unchanged at 15 dead / 1 missing.
  • 3 October 2026: In the National Assembly on 2 October, lawmakers pressed the government to repair flood-damaged roads and bridges before the festival season; Gomadevi Timilsina raised cargo containers swept away by the Bhotekoshi flood and traders needing relief (OnlineKhabar, 2 October). The 6 MW Relekhola hydropower project in Myagdi has stopped generating after rain and floods on 24–27 September damaged its dam, project chief Darshan Kafle said (OnlineKhabar, 2 October). Himlung toll unchanged at 15 dead / 1 missing; flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 2 October 2026 (evening): Bailey-bridge foundations on both banks at Betrawati are complete and installation is under way on the Galchhi–Betrawati road (Minister Sunil Lamsal via OnlineKhabar, 2 October). Nepal’s environment ministry is taking comments on a draft National Climate Policy–2083 ahead of COP31 (November, Türkiye); civil-society groups say it is being rushed and should absorb lessons from the Bhotekoshi flood (The Kathmandu Post, 1 October). Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 2 October 2026: A temporary track on the flood-damaged Galchhi–Betrawati road, the main route towards Rasuwa, reopened to public movement on 1 October; two Bailey bridges are being installed with Nepal Army support and are targeted for completion within a week, while levelling and gravelling remain unfinished (Infrastructure Minister Sunil Lamsal via OnlineKhabar, 1 October). Himlung toll unchanged at 15 dead, 1 missing. Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 1 October 2026 (night): Eight more bodies are recovered at Himlung base camp on 1 October, taking the avalanche toll to 15 dead with one of the 16 Nepali workers still missing; six were flown to Phu village and two to Chame (Manang Assistant CDO Krishna Prasad Poudel via OnlineKhabar and The Kathmandu Post). Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 1 October 2026 (evening): The direct Nuwakot–Rasuwa road link remains cut; Galchhi–Syabrubesi road project chief Krishna Nath Ojha expects a cliff track to reach the Phalaku Khola section by 2 October, with 73 m and 76 m Bailey bridges planned. The Lamjung–Manang link is also still blocked, while the Prithvi and BP highways have reopened (The Kathmandu Post, 1 October). Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 1 October 2026: About 1,000 of the roughly 4,500 people who first sheltered in flood camps remain; no displaced family has yet received the promised Rs 15,000-a-month rent support or Rs 50,000 settlement aid, pending local-unit verification (NDRRMA spokesperson Shanti Mahat via The Kathmandu Post, 30 September). Foreign Minister Shisir Khanal says the US and UAE announced flood assistance at the UN, amounts undisclosed. Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 30 September 2026 (late night): Three more bodies are recovered at Himlung base camp (Aash Gurung, Suraj Rai, Kalam Budha), taking the avalanche toll to 7 dead and 9 missing (Manang CDO Mukti Prasad Khanal via OnlineKhabar; Nepal News). The Energy Ministry says the flood has knocked about 430 MW off the national grid; the NEA has set up a task force on alternative supply before winter (OnlineKhabar). Flood tracker still uses NDRRMA’s 1,453 dead / 5,285 missing.
  • 30 September 2026 (night): Nepal Police Headquarters reports 1,454 bodies recovered and 4,718 missing from the Bhotekoshi flood, 1,334 bodies managed after DNA sampling; the gap with NDRRMA’s last 5,285 missing is unexplained, so the tracker keeps NDRRMA figures for now. The Energy Ministry puts flood damage at 14 hydropower projects (783 MW) and an initial Rs 134 billion, with licence extensions and concessional loans under discussion pending the PDNA (OnlineKhabar, 30 September 2026).
  • 30 September 2026 (evening): Bagmati Province Chief Minister Kiran Thapa Magar asks the other six provinces to support Bhotekoshi flood reconstruction in 15 affected local units and will put a joint proposal to the 7–9 October chief ministers’ meeting. The AIIB Doha meeting ends with Finance Minister Wagle elected a Board of Governors vice-chair for 2026–27; no reconstruction financing amount announced. Flood toll unchanged at 1,453 dead / 5,285 missing (Nepal News; OnlineKhabar; Republica, 29 September 2026).
  • 30 September 2026: Heavy snow on 29 September halted the Himlung avalanche search; 4 dead and 12 missing remain the confirmed figures (NNMGA via ETV Bharat). NDRRMA chief Dharmaraj Upreti told The Kathmandu Post the ~5,285 Bhotekoshi missing are being processed for legal declaration as deceased to release Rs200,000-per-death relief, and that daily flood-data sharing with China and RIMES satellite access have begun. Flood toll unchanged at 1,453 dead / 5,285 missing.
  • 29 September 2026 (evening): NDRRMA puts the toll from the 24–27 September rain at 27 dead and 4 missing across 542 incidents, most of the deaths in landslides. In Manang, a landslide-dammed lake on the Marsyangdi at Ghattekhola near Chame is being drained with excavators after Nepal Army engineers could not find a safe blasting point; roads, power and communications in the area remain cut. The Rasuwa flood toll is unchanged since NDRRMA’s 26 September update (NDRRMA via OnlineKhabar and Nepal Press; Peoples’ Review).
  • 29 September 2026: The Himlung avalanche count firms up: four bodies (Chhebi Bhote, Pasang Bhote, Birendra Gurung and Ghanshyam Rai) have been recovered and identified, and 12 people are still missing as a Nepal National Mountain Guides Association team continues the search by helicopter from Chame. The Rasuwa flood toll is unchanged since NDRRMA’s 26 September update (NNMGA President Tul Singh Gurung via Kathmandu Post/Asia News Network).
  • 28 September 2026 (evening): AIIB President Zou Jiayi, meeting Finance Minister Wagle in Doha, pledges project-preparation grants from the bank’s Project Preparation Special Fund and highly concessional loans for Nepal’s post-flood reconstruction, with no amount announced. The Himlung search resumes by helicopter in clearer weather; the number still missing is unconfirmed after some workers reported out of contact reached safety. Flood toll unchanged since NDRRMA’s 26 September update (Nepal News; OnlineKhabar; Peoples’ Review).
  • 28 September 2026: An avalanche on the morning of 27 September buries the Himlung Himal base camp (7,126 m) in Manang district near the Tibet border; two Nepali guides are confirmed dead and about a dozen support staff remain missing (reported counts range from 10 to 14) as snow and rain delay helicopter searches. Nepal Police put the four-day rain toll at 15, and the Narayani peaked at 11.94 m at Devghat. The Rasuwa flood toll is unchanged since NDRRMA’s 26 September update (Manang district officials via OnlineKhabar; AFP/BBC via The Business Standard; Nepal News).
  • 27 September 2026: Late-season rain kills at least 14 people across Nepal in 72 hours, including four each in landslides in Myagdi and Baglung; the Narayani River crosses its 9-metre warning level, and fresh rain in Rasuwa and Nuwakot compounds conditions for displaced families in temporary camps. The flood toll itself is unchanged since NDRRMA’s 26 September update (ANI via The Tribune).
  • 26 September 2026 (II): As rain returns to Rasuwa and Nuwakot, displaced families in holding centres report leaking tents and wet bedding. A Rasuwa district committee has identified potential resettlement land and sent recommendations to the central government; NDRRMA chief executive Dharam Raj Uprety says land from Syaphrubesi and Timure to Bidur has been surveyed for permanent, safer settlement options, pending a central decision (Kathmandu Post).
  • 26 September 2026: One month on, NDRRMA puts Nepal’s toll at 1,453 dead and 5,285 missing, with 13,795 rescued. Only 112 of the recovered bodies have been identified and handed over; 1,329 DNA samples from remains and 2,060 from relatives have been collected, and 1,113 displaced people remain in 21 holding centres (NDRRMA via PTI/The Tribune).
  • 21 September 2026 (II): Nepal’s government signals it will skip a formal donor conference for reconstruction — the model used after the 2015 earthquake — in favour of bilateral talks with individual donors. A senior Finance Ministry official said Nepal wants to “generate funds through bilateral negotiations with major donor countries like India, China, the US, Japan, South Korea, European nations, and others,” while Amrit Lamsal of the ministry’s International Economic Relations Division said funding could come through “bilateral negotiations and correspondence.” Finance Minister Swarnim Wagle is pursuing commitments on a run of visits, including planned stops in Doha, New York and Washington DC through September–October 2026, ahead of a fuller post-disaster needs assessment still expected within about a month of early September (Kathmandu Post, 21 September 2026).
  • 21 September 2026: Nepal’s NDRRMA revises the toll to 1,451 dead and 5,786 missing (incl. 636 foreign nationals) — the missing count falling from 6,145 on 18 September as DNA identification of recovered remains reclassified some of the unaccounted. Also reported: 13,784 rescued, over 20,900 security personnel still deployed, DNA samples taken from 530 unidentified bodies, and 1,231 displaced people at 20 holding centres (NDRRMA via Qazinform).
  • 11 September 2026 (II): Clarification on climate finance — the US$20 million earlier reported as a flood-relief application was in fact approved under the Barbados Implementation Modalities from three proposals filed before the flood, and is not yet disbursed. Nepal’s separate 31 August emergency request for Bhotekoshi-specific support remains undecided; the Fund for Responding to Loss and Damage’s board co-chairs said on 10 September they were moving to address it “as rapidly as possible,” with a developing-countries meeting set for 12 September ahead of a board meeting now expected before its original December date (Kathmandu Post, 9–10 September 2026).
  • 11 September 2026: Nepal’s Prime Minister’s Secretariat releases a joint NPC–NDRRMA Rapid Damage and Needs Assessment (10 September) putting total reconstruction and recovery needs at Rs 723.315 billion (about US$4.74 billion) — infrastructure roughly 75% of that, the energy sector hardest hit; a fuller Post-Disaster Needs Assessment and a donor conference are still to come. The missing count is revised down to about 5,130, with 1,377 confirmed dead (Kathmandu Post and IANS, 10–11 September 2026).
  • 10 September 2026: Nepal’s toll rises to 1,377 dead, 5,326 missing and 6,827 injured (Kathmandu Post, 8–9 September 2026, citing NDRRMA). Recovery financing comes into focus: a Rapid Damage and Needs Assessment sets initial damage near Rs 400 billion, the National Planning Commission’s full Post-Disaster Needs Assessment is expected within about five weeks and at least 30% higher, and Finance Minister Swarnim Wagle projects a US$4–5 billion reconstruction bill; Nepal has applied to the UN Fund for Responding to Loss and Damage for an initial US$20 million.
  • 8 September 2026: Nepal’s National Disaster Risk Reduction and Management Authority puts preliminary economic losses from the Bhote Koshi–Trishuli disaster at roughly Rs 387.54 billion (as of 3 September), with early government and expert assessments suggesting a reconstruction bill of Rs 800–900 billion — the first verified damage-cost figures for the event.
  • 7 September 2026: Government of Nepal situation update (5 September) puts recovered bodies at 1,344 with about 5,000 still missing (roughly 600 foreign nationals from about 35 countries) and 13,098 people rescued; Tibet’s Gyirong County reports 43 dead and 519 missing as of 6 September. A Rapid Damage and Needs Assessment counts 37 motorable bridges destroyed, 68 suspension bridges damaged, about 55 km of roads lost and roughly 783 MW of hydropower capacity offline across 13 projects.
  • 6 September 2026: Added detail on the early-warning gap — Nepal’s first public alert reached phones ~38 minutes after the collapse (Kathmandu Post, 2 September) — and a UNDP preliminary estimate of ~2.2 million tonnes of flood debris along the Bhote Koshi–Trishuli corridor (1 September).
  • 4 September 2026: Nepal’s NDRRMA raises the confirmed toll to 1,287 dead and 5,083 missing in Nepal, plus 31 dead and 531 missing in Tibet; the collapsed glacier is identified as Langtang Lirung.
  • 1 September 2026: A post-disaster review reports Nepal’s river-monitoring network was tuned for monsoon floods and could not detect the sudden glacier-collapse flood in time; upstream gauges were swept away before an alert could reach downstream communities.
  • 30 August 2026: A second barrier lake that formed downstream near the Chhochen Khola–Purepu Tsangpo confluence drains out largely without a major breach, after a brief overflow on 28 August prompted a pause in rescue operations.
  • 27 August 2026: USGS analysis clarifies that the seismic signal was generated by the ice–rock collapse, not a tectonic earthquake. Nepal reports at least 270 dead and ~826 missing; Tibet’s Gyirong County reports ~558 missing.
  • 26 August 2026: Glacier and rock collapse near the Nepal–Tibet border blocks the Lhende Khola; the natural dam fails and a flood surges down the Bhote Koshi and Trishuli. Early death tolls (~160) are described as underestimates.
  • March 2026: ICIMOD’s HKH Glacier Outlook 2026 finds ice-loss rates have doubled since 2000.
  • July 2025: A transboundary glacial flood from the Purepu Glacier hits the same Rasuwagadhi corridor, destroying the Nepal–China Friendship Bridge.

Explore More Timelines

People also ask

Can a glacier collapse cause an earthquake?
A large glacier or rock collapse generates seismic waves that instruments record and can assign a magnitude to, but that is not a tectonic earthquake. The energy comes from a mass sliding and falling, not from a fault rupturing. In the 2026 Nepal–Tibet event, the USGS concluded the magnitude-5.2 signal was produced by the collapse itself.
Was Chamoli a GLOF?
No. Early reporting suggested a glacial lake outburst, but a 2021 study in Science established that about 27 million cubic metres of rock and glacier ice detached from Ronti Peak and became a debris flow. No lake was involved.
How many people depend on Himalayan glaciers?
ICIMOD says the Hindu Kush Himalayan cryosphere feeds river systems whose water resources are important to nearly two billion people. That does not mean two billion people rely on glacier melt directly — monsoon rain, groundwater and snowmelt also feed those basins — but it is the scale of the region’s downstream population.
Is the Nepal–Tibet flood the deadliest Himalayan glacier disaster?
Yes, by a wide margin. Nepal’s NDRRMA (via IANS) and Chinese state-media updates from 5 October / 6 September 2026 put the combined toll at roughly 1,498 dead and about 5,804 missing across Nepal and Tibet — far higher than Chamoli (200+ dead), South Lhonak (about 55–100 dead) or any other event on this page. Final figures will still be revised as search and recovery continue.
Why did the same area flood in both 2025 and 2026?
The Lhende–Bhote Koshi–Trishuli corridor drains a heavily glacierised, rapidly warming stretch of the Tibetan plateau edge. In July 2025 a supraglacial lake on the Purepu Glacier drained suddenly; in August 2026 a glacier and rock mass collapsed and dammed the river. Different mechanisms, same vulnerable valley.

Frequently asked questions

What exactly happened on 26 August 2026 at the Nepal–Tibet border?
At about 08:40 local time, satellite imagery indicates a large section of the lower end of a glacier detached at roughly 5,200 metres on the Tibetan side and fell about 1,200 metres, gathering rock and sediment. The resulting ice–rock avalanche struck the Lhende Khola, temporarily blocked it, and when the natural dam failed a debris flood surged down the Bhote Koshi and Trishuli rivers.
Was it an earthquake or a glacier collapse?
A glacier collapse. The USGS first reported a magnitude-4.4 earthquake north of Kathmandu, then revised its analysis after studying nearby seismic data, long-period waves and satellite imagery, concluding that no earthquake occurred and the magnitude-5.2 seismic signal was generated by the mass movement.
How far did the flood travel and how fast did the river rise?
The surge moved down the Lhende Khola, Bhote Koshi and Trishuli through Nepal. River monitoring reported by ICIMOD and news agencies indicates the Trishuli rose by as much as nine metres in about thirty minutes.
How many people died in the 2026 Nepal–Tibet flood?
As of 16 September 2026, Nepal’s disaster authority reported 1,403 bodies recovered and 6,150 missing in Nepal — the missing count revised sharply upward from 5,179 the day before after fuller district-level verification — with a further 43 dead and 519 missing in Tibet as of 6 September 2026, a combined toll of roughly 1,446 dead and about 6,669 missing. These figures have risen sharply since the collapse and may still be revised.
Why were so many foreign tourists caught in the flood?
Late August is trekking season in the Langtang and Rasuwa areas near the affected corridor. As of 16 September 2026, Nepali officials reported 607 foreign nationals missing from 34 countries; Chinese authorities reported about 261 foreign nationals from 23 countries among the missing on the Tibetan side. Authorities have not published names.
Is this a glacial lake outburst flood (GLOF)?
Not on current evidence. A GLOF requires a glacial lake as the source. The 2026 event’s primary trigger was a glacier and rock collapse; the flood came from a temporary river blockage failing. It is better described as an ice–rock avalanche that caused a river-blockage flood.
What is the difference between a GLOF and a glacier avalanche?
A GLOF is the sudden release of water from a glacial lake. A glacier or ice–rock avalanche is a mass of ice and rock detaching from a slope. An avalanche can cause a GLOF if it lands in a lake, and it can cause a flood directly if it dams a river — but the two mechanisms are distinct.
What caused the Chamoli disaster in 2021?
About 27 million cubic metres of rock and glacier ice detached from the steep north face of Ronti Peak in Uttarakhand on 7 February 2021. It became a highly mobile debris flow that swept down the Ronti Gad, Rishiganga and Dhauliganga valleys, killing more than 200 people and wrecking two hydropower projects. It was a rock–ice avalanche, not a GLOF.
What caused the Sikkim flood in October 2023?
Peer-reviewed research found that an unstable lateral moraine mass — up to 14.7 million cubic metres of frozen material — collapsed into South Lhonak Lake, generating a roughly 20-metre wave that breached the frontal moraine and released about 50 million cubic metres of water. It was a true GLOF, and it destroyed the Teesta III dam.
What caused the Thame flood in Nepal in 2024?
ICIMOD determined that a rock avalanche hit a glacial lake at about 4,900 metres, producing a displacement wave that breached the lake. The outflow fell about 120 metres, struck a second lake, and breached its moraine dam too — a two-lake cascade that destroyed 14 buildings in Thame village.
What was the July 2025 Rasuwa flood?
A transboundary flood that came down the Lhende River from a supraglacial lake on the Purepu Glacier in China’s Gyirong County, crossed into Nepal at Rasuwagadhi, and killed at least nine people. It destroyed the Nepal–China Friendship Bridge and damaged hydropower and border facilities — the same corridor that flooded again in August 2026.
Did climate change cause these disasters?
For most individual events, climate change is described as a contributing factor to the underlying risk rather than a proven sole cause. South Lhonak 2023 is the exception, with peer-reviewed work directly linking climate-driven glacier retreat and permafrost degradation to the hazard. The 2026 event has not yet been formally attributed.
How does glacier retreat increase disaster risk?
As glacier ice thins and retreats, it stops buttressing steep valley walls, exposes fractured rock, changes stress on slopes, and lets meltwater into cracks. Retreat also opens space for new glacial lakes to form and grow behind unstable moraine dams.
Why does melting permafrost destabilise mountains?
In high mountains, ice within rock fractures acts like glue holding rock masses together. When warming thaws that ice, the rock loses cohesion and becomes more prone to failure. Permafrost was present in the South Lhonak failure zone and is considered a likely contributor there.
Can glacier disasters be predicted?
Not with precision. Monitoring can identify dangerous lakes, measure creeping slopes and track glacier changes, which improves preparedness. But the exact timing of a sudden ice or rock collapse cannot currently be forecast days in advance.
Why are hydropower projects so vulnerable?
They are built in steep, narrow river valleys for the energy potential, which is exactly where glacier-linked floods and debris flows travel. Rishiganga, Tapovan, Teesta III and Rasuwagadhi were all damaged or destroyed in the events on this page.
Are Himalayan glaciers melting faster than before?
Yes. ICIMOD reported in March 2026 that ice-loss rates across the Hindu Kush Himalaya have roughly doubled since 2000, with acceleration after 2010. Its 2023 assessment, using a different metric, found mass loss was about 65% faster in 2011–2020 than in the previous decade.
How much ice have Himalayan glaciers lost?
ICIMOD’s March 2026 reports cite up to about 27 metres of ice-thickness loss since 1975 across monitored glacier datasets, and roughly a 12% loss of glacier area between 1990 and 2020. These are regional aggregates, not a single rate for every glacier.
Can a landslide really register as a magnitude-5.2 seismic event?
Yes. Seismic magnitude measures recorded ground motion regardless of source. Large, fast mass movements radiate seismic waves; the 2026 collapse registered as magnitude 5.2, while the smaller 2022 Marmolada collapse registered around magnitude 0.6.
How many glacial lakes in the Himalayas are dangerous?
There is no single meaningful number without specifying the country, dataset and risk classification. Government and ICIMOD studies for India, Nepal and the wider region identify subsets of potentially dangerous glacial lakes, but Thame 2024 showed that a lake not on any danger list can still cause serious damage.
What is the Hindu Kush Himalaya?
A high-mountain system spanning eight countries, much larger than the Himalayan range alone. Its glaciers and snow feed ten major Asian river basins, which is why it is called the “Water Towers of Asia.”
Did the 2026 flood affect India?
The confirmed damage was concentrated in Nepal and Tibet. Any downstream alerts, water-level changes or evacuations in India should be taken from official Indian agencies such as the Central Water Commission and NDMA rather than assumed from the scale of the upstream event.
What is a debris flow, and why is it called “liquid concrete”?
A debris flow is a dense, fast mixture of water, mud, sand, boulders, ice and wreckage. The very high sediment load makes it far heavier and more destructive than clear water, which is why witnesses describe it as liquid concrete. The phrase is descriptive, not a formal classification.
How is this page kept up to date?
The timeline is revised when there is a material change: a confirmed cause determination, a significant casualty revision, a major rescue development, new satellite evidence or a formal attribution result. Minor one-person changes in casualty counts do not trigger an update.

Related timelines on AiTimeline

✍️ Editorial note & sources

This is an editorial, AI-assisted explainer compiled from public sources and updated as a living page. It is not disaster-response guidance; for safety information follow your national disaster-management authority.

How we classify events: each disaster is labelled GLOF, ice–rock avalanche, landslide-dammed flood or debris flow based on the best available post-event science. If research revises a classification, we update the entry.

Primary sources: US Geological Survey (USGS); International Centre for Integrated Mountain Development (ICIMOD), including the HKH Glacier Outlook 2026 and the 2023 HKH assessment; peer-reviewed studies in Science (Chamoli 2021) and Landslides (South Lhonak 2023); Nepal’s National Disaster Risk Reduction and Management Authority; Chinese state media for Tibet figures. Reporting sources: Reuters, Associated Press, Al Jazeera, BBC, France 24 for current-event detail. Figures for the 2026 event are preliminary and were changing at the time of writing.

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