· &nbsp;At least 400 people are dead or missing after heavy rainfall lashed arid regions of northwestern Pakistan. Walls of mud and boulders engulfed entire villages in Khyber Pakhtunkhwa Province. More than 700 people have been killed in floods in Pakistan since June.&nbsp; · &nbsp;Over in India’s Jammu and Kashmir at the same time, multiple slurry floods on 17-18 August killed more than 80 people · A mudslide possibly caused by a glacial collapse upstream in Uttarakhand on 5 August nearly wiped the village of Dharali off the map. At least 70 people, 23 of them Nepalis are dead or missing. · On the night of 8 July, <a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof">glacial lakes in Tibet overflowed</a>. By dawn the mudflow had demolished the Nepal-China border bridge killing at least 11 people, destroyed hydropower plants, swept away bridges, roads, over 100 cargo trucks and newly imported electric vehicles. All these disasters have a common thread: a cascade of hazards caused by record-breaking rainfall on fragile Himalayan slopes destabilised by melting glaciers and permafrost, seismicity and poorly engineered infrastructure. They are called ‘rain bombs’ — a heavy localised downpour measuring more than 100mm/h on a steep mountainside. As global warming heats the atmosphere, warmer air can hold more water vapour. The heavy rain then falls where there should be snowfall: on moraines and slopes that have lost the permafrost adhesive that held the debris together. “Increasingly, there is now more rainfall at higher altitudes where there used to be snowfall previously, and this directly impacts loose material in that fragile landscape which moves down,” explains Mohan B Chand, a Himalayan Glaciologist at Kathmandu University. “Moreover, the rains these days are heavy and fall within a few hours. So even a small burst has bigger impact.” The <a href="https://nepalitimes.com/banner/drones-to-the-rescue-in-melamchi">2021 Melamchi flood</a> and the <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">Sikkim disaster in 2023</a> have been attributed to record-breaking torrential rain on a glacial moraine that collapsed, unleashing a catastrophic debris flow.&nbsp; The Bhote Kosi flood this year happened even without torrential rain, and originated at rapidly expanding supraglacial lakes that overflowed, similar to what happened on the Mendenhall Galcier in Alaska last week. In Uttarakhand, the trigger could be in the upper catchment cryosphere, or a landslide dammed lake. Basanta Raj Adhikari of the Centre for Disaster Studies at the Institute of Engineering also calls them ‘sediment bombs’. He clarifies: “There is lots of sediment up there from landslides or glacial activity, and when there is heavy rainfall and hotter temperature, they are unleashed downstream. One thing is for sure, these extreme events are getting more frequent and more destructive.” Researcher Alton C Byers who has studied melting glaciers in the Himalaya and Andes names the eight most potentially dangerous glacial lakes in Nepal: Lower Barun, Chamlang North Tso, Chamlang South Tso, Dig Tso which burst in 1984, Lumding Tso, Thulagi, Tso Rolpa and Imja Tso (see map).  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250822030844_70b3bf6a1ad9b9f9481c9af860629b2a05ac1338a3b89a831506f1c6bdddf5ec.jpg" data-media-id="editor_3" data-image-id="20250822030844_70b3bf6a1ad9b9f9481c9af860629b2a05ac1338a3b89a831506f1c6bdddf5ec" data-rendition-name="original" width="522" height="557" loading="lazy" alt="high risk glacial lakes in Nepal"> </figure>  Of these, Tso Rolpa and Imja have been lowered by 3m each, while Thulagi, Lower Barun, Lumding Tsho, and Hongu 2 glacial lakes have been targeted for lowering by the Department of Hydrology and Meteorology as part of the recent Green Climate Fund grant of <a href="https://nepalitimes.com/here-now/meltpools-in-the-himalaya" target="_blank">$36.1 million awarded to Nepal</a>. “These lakes have changed over the years as their debris-covered glaciers continue to recede,” Byers told Nepali Times. “When water volume in the lake basin increases, they become more vulnerable to flood triggers such as overhanging ice as glaciers recede further to their headwalls, and permafrost on their moraines continues to melt.” <h2>These are not ‘natural disasters’</h2> Scientists have given the current planetary epoch a name: the Anthropocene. And anthropogenic causes in this era heighten the risk of disasters. Indeed, an analysis of recent Himalayan calamities (page 1) shows that there is much more at play here than climate breakdown. Haphazard encroachment of floodplains, quarrying and crusher activity exacerbated the effect of <a href="https://nepalitimes.com/editorial/when-it-rains-it-pours-ksqprbu3">extreme rainfall on 28 September around Kathmandu Valley</a> that killed 200 people. The human cost of the 5 August catastrophe in Uttarakhand would have been high in any case, but the fact that the tiny village had expanded across a vulnerable alluvial fan to cater to a tourism boom meant more death and destruction. There are similar alluvial fans across Nepal, where small towns have expanded because new highways follow rivers, like Beni located at the confluence of the Myagdi Khola and Kali Gandaki. Other towns like Kagbeni or Damauli are located on the banks of rivers and tributaries that are directly downstream from rapidly expanding glacial lakes or unstable mountains. “In Butwal, people are building houses on the floodplain of the Tinau River, and yet people blame climate change or rainfall when there is a disaster,” says Basanta Raj Adhikari at the Institute of Engineering. “This is happening all over the country. Imagine the kind of devastation Beni would suffer if there was a big flood.”  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250822030848_ed411f8618c7a411ed4c165e91f3b880abb085a8a511405710dd8220f657da84.jpg" data-media-id="editor_6" data-image-id="20250822030848_ed411f8618c7a411ed4c165e91f3b880abb085a8a511405710dd8220f657da84" data-rendition-name="original" width="1200" height="800" loading="lazy" alt="Beni Bazar"> <figcaption>RISKY CONFLUENCE: Beni has expanded rapidly after the highway to Mustang was built. But the town is situated on the alluvial fan of past flash floods on both the Kali Gandaki and Myagdi Khola which have dangerous glacial lakes in their upper catchment. Photo: BENI TOURISM</figcaption> </figure>  Traditionally, Nepal’s villages and settlements were located high above rivers because our forebears learnt lessons from recurring flash floods. Now, the road network follows rivers, and towns have sprung up along these highways. Even when roads are not on river banks, many gouge out slopes above, unleashing massive landslides that block rivers. Experts say Nepal’s hazard map should now be updated for glacial outbursts so municipalities can plan risk-sensitive land use zoning. This &nbsp;must go hand-in-hand with measures to reduce the risk by structural mitigation, such as engineering and construction, and then with risk awareness and early-warning systems. Says Himalayan researcher Alton C Byers: “Sooner or later, communities will realise that certain sites are simply no longer safe for a village or city, especially because of climate change in the mountains. The Himalaya has always been high-risk with its steep slopes, thin soil, monsoon rainfall regime, and frequent seismic activity. So, some places are no longer safe to live in.” Mohan B Chand of Kathmandu University adds that <a href="https://nepalitimes.com/banner/climate-smarter-himalayan-infrastructure">hazard mapping is especially crucial for expensive hydropower plants</a>: “Most of these are on snow-fed rivers, but environmental risk assessment is not taken seriously.” He says that because Nepal is set to generate 28,500MW by 2035 to meet its carbon neutral target, the government must work to minimise upstream risk by integrating disaster mitigation components in new energy investments. Few know that Nepal’s first hazard mapping was done 40 years ago in the Khumbu with a United Nations University study titled ‘Highland Lowland Interactive Systems’. It is hard to find that document anywhere. Today, hazard mapping technologies, satellite remote sensing, drones, synthetic aperture radar (SAR) and modelling with AI have made it much easier to integrate multi-hazard risk assessment. That data needs to be made available to local governments so they can plan. Cell phones and new apps that monitor real-time glacial lake levels, live precipitation and hydrological data, and local weather forecasts can make early warning systems more effective. Recent disasters have shown that even the smallest of glacial lakes that are rarely considered in risk assessments can cause much damage. Langmale Lake in the Barun Valley was less than 0.1 km2 in size, but <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting" target="_blank">the flood in 2017</a> caused extensive downstream damage. The 2012 Seti flood in Pokhara, the Chamoli disaster in Uttarakhand in 2021, the South Lhonak proglacial lake burst in Sikkim in 2023 that washed away the $1.7 billion Chungthang Teesta III Project, and the August 2024 floods above Thame in Khumbu are other recent examples.&nbsp; Byers thinks some of these floods may have been initially triggered by massive rockfall or moraine collapse related to <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost" target="_blank">melting permafrost</a>. The size of a glacial lake alone does not determine the severity of destruction. What makes all the difference is downstream development, and if there pre-warning. Dig Tso in Khumbu which burst in 1984, was much larger than the lake that caused the Bhote Kosi flood in July, but the economic cost to the country of the trans-boundary disaster this year was much higher. Says glaciologist Chand: “We have to monitor the lakes, not just via remote sensing but with field visits. These may be costly, but mitigating the risk is less expensive than the disasters themselves.” Nepal has the technology and trained personnel to do hazard mapping, monitoring, and to design early warning apps. That data and information now needs to be available to all three levels of government to improve preparedness and risk reduction. “The cascading and compounding hazards are increasing in the Himalaya, this must be the subject of our research now,” says Adhikari at the Centre for Disaster Studies. “Recent events are a wake-up call, if we do not take this seriously things may be more dangerous in future.”

Sonia Awale

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Rain bombs

<a href="https://nepalitimes.com/banner/including-local-knowledge-to-study-climate-change">Alton Byers</a> has organised frequent research expeditions to the Himalaya for more than 50 years. Recently, he returned to the <a href="https://nepalitimes.com/banner/tracing-past-glacial-floods-in-kangchenjunga">Kanchenjunga region</a> which he has visited three times since 2019. His team was there to gather more data for an ongoing study of glacial, ecological and socioeconomic changes in the region. But, his attention was soon diverted when a young man from the local community told Byers that locals had noticed large meltwater ponds forming at the toe of the <a href="https://nepalitimes.com/here-now/saving-kangchenjunga">Kanchenjunga</a> Glacier, upstream from Ghunsa and Kambachen. “He asked if we could go take a look at it,” Byers said. “We were on our way up to the Kanchenjunga base camp, so we made a detour. Sure enough, you could see these considerable lakes, perhaps a half-a-square-mile and growing.” Byers sprung into action. First, he interviewed other community members about the ponds — they confirmed the observations and growing concern. Then, over the ensuing months, he assembled a team of experts to conduct a study of how the ponds were changing. <a href="https://www.mdpi.com/2073-4441/17/10/1457#:~:text=This%20study's%20modeling%20results%20suggest,Ghunsa%20in%20the%20form%20of">The study was published in the journal Water earlier this month</a>. The paper outlines a number of potentially dangerous flood scenarios that could be triggered at the site in the future. The researchers urge regional authorities to implement mitigation measures, including a monitoring program and an early warning system for flooding.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3.png" data-media-id="editor_4" data-image-id="20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3" data-rendition-name="original" width="1967" height="2128" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Predicted future Kanchenjunga proglacial lake extent and depth, frontal moraine, and potential avalanche location, which were used as input for modeling the GLOF cascade in r.avaflow. The background image is from Google Earth Imagery taken on 25 December 2020.</figcaption> </figure>  Byers’ first call for collaboration was to <a href="ttps://www.icimod.org/team/sonam-wangchuk/">Sonam Wangchuk</a>, an expert in snow and ice research via satellite imagery at the International Centre for Integrated Mountain Development. The images were striking. From 2022 to 2024, the ponds grew from puddles to large, interconnected bodies of water.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b.png" data-media-id="editor_6" data-image-id="20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b" data-rendition-name="original" width="1861" height="2126" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Evolution of supraglacial lakes on debris-covered glacier (27.7726, 88.0187) at Kanchenjunga. Time series satellite composite images were acquired by Sentinel-2 Multispectral Instrument between September and October, with the exception of the April–May 2024 images. Two large and distinct lakes which expanded rapidly in 2022 and continued to grow in 2023 and 2024 are labeled as 1 and 2, for locational comparison with the oblique view taken on 25 May 2024. Photo: ALTON BYERS</figcaption> </figure>  “It’s sort of an indicator of how these melting processes are accelerating,” Byers said. Next, Byers and collaborators estimated that the meltwater ponds could form a large glacial lake. That lake, if it forms, will be vulnerable to <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">outburst flooding</a>, which could be triggered by melting processes, structural collapse or rockfall from surrounding slopes. Finally, the researchers focused their efforts on modeling potential floods. They identified four scenarios, from small to large.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae.png" data-media-id="editor_8" data-image-id="20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae" data-rendition-name="original" width="2637" height="3197" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Flood extent under various scenarios: areas impacted by all four GLOF scenarios are labelled as 4, those affected by three scenarios as 3, by two scenarios as 2, and by only one scenario as 1. (B) Hydrograph generated from GLOF modeling in r.avaflow and used as the input flow data for modeling each GLOF scenario in HEC-RAS. Flow depth and velocity at Kampachen (C,D) and Ghunsa (E,F). Discharge rate and time of peak, and flow arrival at Kampachen (G) and Ghunsa (H) under different scenarios.</figcaption> </figure>  Under the mildest scenario, the flood surge would travel 100km down the Tamor River, and under the worst-case scenario it would travel at least 220km with impact on houses and bridges, livestock, crops and tourism infrastructure. Byers warns that without adequate preparation, glacial outburst flooding can be deadly. The paper advises local and regional authorities to take measures to prevent a flood originating from the study site. Their recommendations include establishing early warning systems for flooding, partnering with research organisations in Kathmandu to monitor the site and adapting zoning laws to prevent new buildings in flood zones.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58.jpg" data-media-id="editor_9" data-image-id="20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58" data-rendition-name="original" width="1356" height="668" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Imja Lake, a glacial lake in the Mount Everest region of Nepal, began as meltwater ponds in 1962 and now contains 90 million cubic meters of water. Its water level was lowered to protect downstream communities. Photo: ALTON BYERS</figcaption> </figure>  Read also: <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">The not-so-permanent frost</a>, Wilfried Haeberli and C Alton Byers One of the cheapest and most effective early warning systems is deceptively simple: cell phones. Says Byers: “Not everyone can afford multi-million dollar early warning systems that rely on laser readings of water depth. But, studies have shown that cell phones, at least during the daytime, are one of the better early warning systems out there.” Byers hopes the study can help the same people that brought the issue to his attention: “The goal was always to share the research with the local community. Then they have all of the information they need to make the best decisions possible.” <a href="https://www.colorado.edu/instaar/2025/05/27/researchers-model-dangerous-glacial-lake-himalayas-and-propose-solutions">Gabe Allen</a> is Senior communications specialist at the Institute of Arctic and Alpine Research at the University of Colorado Boulder.

Mapping Kangchenjunga glacial flood risk

<a href="https://nepalitimes.com/banner/human-face-of-a-himalayan-climate-crisis" target="_blank">Janmu Sherpa</a> was a grandmother with a dozen goats and a tea house in Donggang in the Rolwaling Valley. Her stopover served trekkers en route to Tso Rolpa Glacial Lake and the trail over Tashi Laptsa Pass to Khumbu. In 2018, I spent months in the Rolwaling Valley studying how <a href="https://www.ted.com/talks/rastraraj_bhandari_what_climate_activists_are_doing_wrong" target="_blank">mountain communities perceive</a> climate change. Unlike my climate-anxious self, Janmu was calm, even hopeful, despite having lived through floods, landslides, and the 2015 earthquakes. “No one knows when Tso Rolpa will burst, so we cannot stop our daily chores. Let fate decide,” Janmu Sherpa had said. Last year, fate did decide. On 22 June 2024, the Dorji Phungmo Glacial Lake burst. The resulting flood swept through the Rolwaling River, washing away homes and hotels in Donggang. Janmu <a href="https://thehimalayantimes.com/nepal/climbers-valley-devastated-by-floods-immediate-relief-sought" target="_blank">was among</a> the missing, and later declared dead.&nbsp; I learned of her disappearance during a recent cycling trip through Panauti along the <a href="https://nepalitimes.com/multimedia/a-flood-of-tears-on-the-rosi" target="_blank">Rosi Khola</a>, which was devastated by deadly flash floods on 28 September 2024.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918054_14898953b7a5808b51440f7a6fa35a7d66146bbb1d62bf88729a83a558ca8ebf.jpg" data-media-id="editor_4" data-image-id="2025051918054_14898953b7a5808b51440f7a6fa35a7d66146bbb1d62bf88729a83a558ca8ebf" data-rendition-name="original" width="1500" height="1000" loading="lazy" alt="A pre-monsoon déjà vu"> <figcaption>Tso Rolpa glacial lake at 4,580m has grown seven times in size in the past 60 years due to global warming. </figcaption> </figure>  Tipper trucks rumbled through the dusty road, carrying stones and gravel from unregulated quarries and sand mining along the Rosi. This was destruction disguised as development, and the crusher industries had <a href="https://nepalitimes.com/news/the-revenge-of-the-rivers" target="_blank">magnified the impact of record rainfall</a>. On the other side of the mountain, along the Lele and Karmanasa Khola, families are still reeling from last year’s floods. Here, too, a quarrying frenzy exacerbated the <a href="https://nepalitimes.com/banner/nepal-valley-suffers-quadruple-disaster">destructive power of the floods</a>. There are thousands of untold stories like Janmu, and the estimated 200 who perished in the September floods. Most have been forgotten, their deaths blamed on fate. I write this from afar, as Kathmandu hosts the Sagarmatha Sambaad this week to draw global attention to the impact of the climate crisis on the Himalaya. The summit took place as pre-monsoon rains lashed the Rosi and Lele Valleys. Even before the start of the rainy season, more debris flows from the mining operations destroyed repaired roads and neighbourhoods rebuilt after floods last year. The rivers that flooded Kathmandu in September 2024 are still vulnerable. Aside from a few sandbanks built by local hands, nothing has changed. No national reckoning. No systemic response. Instead, everything is blamed on climate change.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918054_57fa57586b1e370e715daf837aa4cae3e73b0f029bb0ccef8be768e85656cc5f.jpg" data-media-id="editor_7" data-image-id="2025051918054_57fa57586b1e370e715daf837aa4cae3e73b0f029bb0ccef8be768e85656cc5f" data-rendition-name="original" width="1499" height="1000" loading="lazy" alt="A pre-monsoon déjà vu NT"> <figcaption>Janmu Sherpa's village of Donggang is directly downstream from Tso Rolpa Glacial Lake.</figcaption> </figure>  <a href="http://as%20kathmandu%20hosts%20the%20sagarmatha%20sambaad/" target="_blank">Janmu Sherpa’s story</a> haunts me not just because of her loss, but because she shaped my journey as a climate activist. She taught me that climate action is not just about carbon or conferences, it is about livelihoods, listening, and the impossible trade-offs faced by communities where survival is more urgent than sustainability. As monsoon clouds gather again, there is a sense of dread not just about floods, but for the apathy that follows. We are trapped in a cycle of climate inaction fueled by corruption, state neglect, and a development model that treats rivers as resources to be drained, not lifelines to be protected. It is no longer a question of if the floods will come, but when, and how devastating they will be. And yet, <a href="https://nepalitimes.com/here-now/politicians-and-cronies-blamed-for-kavre-floods" target="_blank">those in power remain unmoved</a> even when disaster strikes their own backyard. We are still chasing climate finance and hosting international summits, while local insurance markets stagnate and communities fend for themselves. To be sure, global advocacy matters. The Himalayan climate crisis must be on the international agenda. Melting glaciers here affect billions downstream. But adaptation cannot begin and end in air-conditioned conference halls. It must bring real preparedness to villages, valleys, and riverbanks of Nepal.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918058_3ec77114d434385351ad1637fd5ab42dc6a76b94b0e90f1c6e683c71535f6e6a.jpg" data-media-id="editor_10" data-image-id="2025051918058_3ec77114d434385351ad1637fd5ab42dc6a76b94b0e90f1c6e683c71535f6e6a" data-rendition-name="original" width="1701" height="1000" loading="lazy" alt="A pre-monsoon déjà vu"> <figcaption>The Sagarmatha Sambaad climate conference in Kathmandu this week. Photo: PRADEEP RAJ ONTA / RSSseasonmedia2007</figcaption> </figure>  I visited the communities ravaged by floods in September and as I wrote in <a href="https://nepalitimes.com/opinion/flood-of-despair" target="_blank">Nepali Times</a> then, top-down responses are always too little, too late and too ineffective. The only real solution is bottom-up, community-led adaptation. Those who lived through the floods know what needs to be done, and those privileged and in power need to enable them. Community-led adaptation is not just a buzzword. It is our only viable path forward. It means empowering local people with the tools, knowledge, and resources to protect themselves. It means investing in early warning systems that reach the last mile and actually work, restoring ecosystems that buffer floods, and supporting indigenous knowledge that has long helped communities live in harmony with nature. It means letting go of our belief that somehow our degrees in climate change and attendance in global climate conferences enable us to tell communities how they should be responding to climate change. It means shifting power and funding to the grassroots, where resilience is not theoretical — it is lived, practiced, and urgently needed. As the rains return, I am reminded of Janmu Sherpa’s voice of quiet wisdom. Her innate resilience did not save her life. Let us not wait for the next flood to act. Let us protect what we still have. Rastra Raj Bhandari is co-founder and fellow at the Himalayan Water Project, where he leads the research on climate finance opportunities for the Himalaya.

A pre-monsoon déjà vu

In the first two episodes of this series, we looked at how <a href="https://nepalitimes.com/here-now/people-and-mountains-are-thirsty-in-eastern-nepal">climate breakdown has worsened the water shortage in eastern Nepal</a>, with rains failing and springs going dry.&nbsp; But there is a flipside. In the monsoon, there is also the curse of too much rain leading to destructive landslides, floods driving people out.&nbsp; <a href="https://nepalitimes.com/here-now/climate-crisis-drought-food-deficit-migration">Analysing meteorological and hydrological data from the past half-a-century in eastern Nepal’s Tamor River basin</a>, the big floods of 1963 and 1968 stand out with other less destructive monsoons in between.&nbsp; Nepal’s monsoons usually last 112 days from mid-June to mid-September, and its clockwork arrival and departure has inspired Nepali poetry and song. But climate breakdown has disrupted the timetable, and there have been years with highly unusual monsoons and floods. In 1968, the monsoon delivered more rain than usual in some places and less than normal in others, and the big floods actually came after the monsoon is supposed to have retreated.&nbsp; The national news agency RSS reported a damaging flood in Sunsari, the district in the plains where the Kosi River disgorges into the plains after confluence of the Arun, Sun Kosi and Tamor. Three days later, RSS reported that 500 cattle and 1,500 goats had drowned in Sunsari, and a child’s body had been found. And upstream in Leuti Khola, three people and seven houses were swept away. A week later, RSS reported again that seven people and 14 livestock had been killed by floods, and bridges as well as paddy ready for harvest were swept away. Even upstream in Olangchung Gola, three people were killed.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010452_9fe3ea424cd644cb1f5a06a731f44d466d70216f39d943e0bd4a5f6f13fdf90d.jpg" data-media-id="editor_2" data-image-id="20240427010452_9fe3ea424cd644cb1f5a06a731f44d466d70216f39d943e0bd4a5f6f13fdf90d" data-rendition-name="original" width="1688" height="1088" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  Laxmi Prasad Siwakoti was a boy in 1968, and remembers enormous boulders thundering down rivers. One boulder the size of a house luckily was pushed to the banks before it could destroy a key bridge below Taplejung. All this water created even more death and destruction in the inland delta of Sunsari, also washing down the bodies of people and livestock from upstream. The 1968 post-monsoon flow of the Kosi reached 23,106 cumecs – four times the volume in the 1963 flood. Some researchers attributed the 1963 flood to the bursting of Tiptala Glacial Lake in the Kangchenjunga area, and that the 1968 flood was also caused by another moraine collapse on the same lake.&nbsp; But analysis of precipitation data of the Department of Hydrology and Meteorology shows that the reason for the catastrophic floods of 1968 was unusually heavy post-monsoon rainfall in the Tamor basin. Archival records of rainfall at Mulghat below Dhankuta shows that there was 162mm of rain on 3 October and another 158mm on 4 October. This meant that one-third of the total rainfall during four monsoon months fell in just two days. Never had Mulghat recorded so much rain in such a short time, and in the 55 years since there has been that much rain only twice. On 4-5 October 1968, Dhankuta received 300mm of rain. It had never received so much rain in the autumn before or since. Similarly, Taplejung recorded 231mm of rain in the same two days – it has never received so much rain in the post-monsoon since. Hydro-meteorological stations across eastern Nepal in Panchthar, Taplejung, Dhankuta and Sankhusabha all show data of record-breaking post-monsoon precipitation on 3-4 October 1968. In fact data shows that except for northwestern Nepal, there was heavy unseasonal rain all over. Dhulikhel near Kathmandu recorded 221mm rain that day, and even Jomsom in the trans-Himalayan rainshadow got 58% of its annual rainfall in just one week. In a paper titled Heavy Monsoon Rainfall in Nepal, J L Nayava dug up an archival weather map from 1968 that showed a cyclone develop in the Bay of Bengal a week after the official retreat of the monsoon from Nepal in conjunction with a low pressure area over southern India. Both systems moved northwards, and it could have been the combination of the two that dumped the record rainfall in Nepal.&nbsp; Nayava notes: ‘On 29 September, a small low appeared over the Bay of Bengal at about 10°N, 90°E. During the next two days, the circulation of this low expanded as it moved north-eastwards into central India and intensified into a depression. By 3 October, Nepal and much of India had come within the circulation of this depression… During the next two days, a sharp 500mb trough passed through Nepal and central India and as the polar westerlies at 200mb intensified and moved equatorwards, bringing the subtropical westerly jetstreams ever closer to Nepal. As the depression moved north, the anticyclonic circulation at 200mb over the depression intensified and became orientated in a south-west-north-east direction. Associated with these developments, widespread rain fell in most parts of Nepal…’  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010452_6fc01e56307dfd3c43e58d7170346d11a1fd8ee2a748074b22aa84bcfdab8369.jpg" data-media-id="editor_3" data-image-id="20240427010452_6fc01e56307dfd3c43e58d7170346d11a1fd8ee2a748074b22aa84bcfdab8369" data-rendition-name="original" width="1500" height="1000" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  It was not just eastern Nepal that suffered destruction, many people were killed in Bhojpur, Khotang and Solu to the west. If this was indeed a glacial lake outburst flood, the destruction would not have been so widespread. The hydrological data of the Tamor of 3-5 October 1968 are also not commensurate with a flash flood triggered by a glacial lake burst. The Mulghat hydrological stations showed that on 4 October, there was 3,060 cumec of flow (volume of water never recorded before) which decreased only slightly over the next few days and returned to a more normal 636 cumecs only on 9 October.&nbsp; By the time the rains stopped that October, 60 people were dead in Kosi zone alone, thousands of livestock were killed and houses swept away. The new bridge over the Tamor and other suspension bridges were destroyed. But that was not the end of the story. On 29 October 1968 came news that 91 people had been killed in Taplejung, 60 in Terathum, 30 in Panchthar and three in Dhankuta. Just in the Tamor watershed, 184 people were killed and thousands made homeless. Nepalis have learnt over the years to be prepared for disasters during the monsoon, and to breathe a sigh of relief when the rains end. But the 1968 floods hit after the monsoon, when people felt safer. Floods were nothing new in the Tamor. There was an unimaginable one five years earlier on 15 August 1963 that swept away 16 houses in Olangchung Gola, and this flood was different from the one in 1968. Locals remember an air blast preceding the flash flood, and an approaching roar that shook the mountains like an earthquake. Houses shook, cattle cowered and goats ran for cover. Upstream, villagers saw clouds of dust and spray, and there was a smell of gunpowder in the air as enormous boulders collided with each other. Although this was the monsoon period, the precipitation in the day preceding the debris flow was normal. This could not have been caused by a cloudburst. Alton C Byers, the American glaciologist who has researched historical glacial floods in the Kangchenjunga region, used satellite imagery and interviews with local villagers to pinpoint the flood to the bursting of Tiptala glacial lake at 4,900m. “The gunpowder smell and the wind preceded the arrival of the debris flow,” remembers Nil Limbu of Chhiruwa of Taplejung, an eye witness of the 1963 event. “It destroyed everything, took away all the trees, left just rocks and boulders.” The flood washed away the mule trail along the Tamor, and swept away the flat meadow along the river where there used to be a weekly market. Today, the trail is higher above the river, but for years later, there used to be rockfalls from above. The debris flow raced downstream destroying houses, trails, bridges, farms, livestock. The flood made national news, and RSS reported that below Dhankuta, the Tamor destroyed the trail to Taplejung and washed away seven bridges. The glacial lake outburst flood on the Tamor met the Arun and then the Kosi where the river flow spiked to 6,371 cumecs. Further downstream in the plains, the flood destroyed the western embankment of the Kosi Barrage, inundating villages in more than 1m of water. A month later, the government released the death toll: 32 killed, unknown number of livestock, standing crops, and causing damage equivalent to 1.6% of Nepal’s annual budget that year. Nepal’s famous eye doctor Sanduk Ruit’s family also had to leave their home in Olangchung Gola after that flood and settled down in Dhankuta. The combined result of the record rainfall-induced floods of 1968 as well as the glacial lake outburst flood of 1963 could have been early examples of climate-induced floods, which have become more frequent in recent years.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010456_c6e6182935c1704629e175dc351f79b74367824a14be020d0b05bdda201a2747.jpg" data-media-id="editor_4" data-image-id="20240427010456_c6e6182935c1704629e175dc351f79b74367824a14be020d0b05bdda201a2747" data-rendition-name="original" width="1036" height="1184" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  On 17 June 2023 Memeng station in Panchthar recorded 230mm rainfall in a 24 hour period, the highest rainfall ever recorded in that station (second highest was 148mm in July 2002). Nearby Dovan of Taplejung experienced 106mm on 18 June and 102mm on 19 June. The basin-wide floods on the Tamor and its tributaries caused damage worth at least Rs8.5 billion on 30 hydropower plants in Sankhuwasabha, Taplejung and Panchthar. Eighteen workers were killed. Half of these schemes were under construction, but plants generating 130MW were knocked out of action. Some, like the Upper Piluwa Khola 2 and Super Hewa Khola have still not been repaired. While these were all caused by extreme rainfall events, on the Sikkim side of Kangchenjunga a post-monsoon disaster on 4 October 2023 washed away several hydropower plants on Teesta and its tributaries, and killed nearly 100 people downstream. The 1,200MW Chungthang Dam built at a cost of $1billion was destroyed. It was later revealed that extreme rainfall on the South Lhonak Glacial Lake, north of Kangchenjunga, caused the collapse of a lateral moraine which allowed a wave to breach the terminal moraine. The lateral moraine could have been weakened by thawing permafrost, and collapsed during heavy rainfall on the night of 4 October.&nbsp; The Sikkim disaster was an important lesson for Nepal, which has invested heavily in infrastructure on this side of the border. More than a dozen medium and large hydropower plants have been built or are under construction along the Tamor alone. The 1960 Tiptala and the 1980 Nangama glacial lake bursts are further proof that such disasters can happen again without warning because of climate breakdown. Besides droughts and floods, landslides are also the reason many people from eastern Nepal have migrated to the relative safety of the plains. A huge landslide in 1946 in Hangdeva in Taplejung is still displacing many people. East of Hangdeva, another landslide in 1977 killed 25 people and the rest of the village just moved out. It is clear that with the climate crisis, extreme weather events and glacial lake bursts will be more serious and frequent, affecting lives and livelihoods, contributing to outmigration.&nbsp; This is the final of a three-part series supported by the Barbara Foundation.

Either too little, or too much water

From stone spouts to cast-iron mains, Nepal’s water system and its struggle to provide safe water tells a larger story of power, disease, dependency — and lessons for the future. From 1823 to 1891, the Nepali state made just two notable interventions in Kathmandu’s drinking water system. The first was when Prime Minister Bhimsen Thapa commissioned a stone pout (hiti) to tap groundwater within the valley’s traditional supply system. The second came nearly 70 years later with Nepal’s first industrial-era water system, the Bir Water Works in 1891 under Prime Minister Bir Shumsher Rana. Linking these two milestones was the spectre of cholera. From the 19th century on there were seven global cholera pandemics. <a href="https://www.sciencedirect.com/science/article/pii/S0264410X19309995#bb0325" target="_blank">Originating in Asia</a>, the disease reached Europe and the Americas, the Vibrio cholera bacillus breeding in poor sanitation wherever it found it. The first wave erupted in 1817, followed by others in 1829, 1852, 1863, 1881, 1889 and, finally, in 1961, the seventh pandemic which still lingers on. London, the epicentre of the Industrial Revolution, was repeatedly stricken. In Britain ‘miasma’ foul air was blamed. &nbsp;In Nepal, cholera was seen as divine damnation. By the late 19th century, as Nepal’s relationship with Britain deepened, the Bir Water Works was inaugurated in 1891 as a defence against cholera. Whether cholera also shaped Bhimsen Thapa’s decision in 1823 is less clear. Contemporary records note the commissioning of Sundhara, but do not refer to the cholera epidemic raging at the time. The silence itself is telling: Nepal’s elites were ruling in the shadow of the disease. Bhimsen Thapa first resided in Thapathali Palace, which was built in 1802 by Nain Singh Thapa, father of Mathabarsingh Thapa, who would briefly become prime minister in the 1840s. In 1806, Bhimsen Thapa moved to Bagh Durbar, a new complex on the western edge of Tundikhel. Historians are vague about the water supply in the residences of the nobility, but wells and water hauled from rivers, ponds, canals, and other sources were likely the primary sources. A small hiti north of Bagh Durbar, near today’s Sun Dhara, may have supplied the palace. In 1823, Bhimsen Thapa had it enlarged, making it the last and largest state-built hiti in Kathmandu. Even as Bhimsen Thapa was involved in palace intrigues and border conflicts, Britain was engineering pipelines. By the late 18th century, Sir Thomas Simpson had invented the bell-and-spigot joint, making long-distance pipes viable. Fluid dynamics, dealing with pumps, pipes, and filters, was becoming a foundational discipline. In Kathmandu, the scourge continued. Cholera struck Kathmandu repeatedly, in 1862, 1867, 1872, 1874 and 1875. The 1872 epidemic, <a href="https://nepalitimes.com/news/kathmandu-in-the-time-of-cholera" target="_blank">according to historian Tom Robertson</a>, claimed between 200 and 250 lives a day. On average, cholera killed between 1,200 and 1,500 people annually in Kathmandu Valley, an enormous toll for its small population. The summer of 1885 was especially calamitous: a cholera epidemic ravaged Kathmandu and its periphery from the beginning of June until late August. The disease even breached the royal palace, reportedly killing 23 people, mostly young girls. Records show that 909 people received treatment at the British Residency dispensary, and estimates suggest that as many as 10,000 people perished in a city of 50,000. In November that year, Bir Shumsher seized power in a coup. He inherited not only a premiership but a Valley ridden with disease. Cholera was endemic, and it was accompanied by typhoid, smallpox, goitre, syphilis, and chronic dyspepsia. The The British Residency dispensary at Lainchaur was inadequate. “In a poor country like ours, wealth means health,” Bir Shumsher remarked, an unusually pragmatic admission that epidemics were not divine punishment but structural afflictions of urban life. He soon pledged to expand health care. In 1889, he opened Bir Hospital and staffed it with Indian doctors to treat cholera, typhoid, smallpox, and other prevalent illnesses. PIPED WATER Bir Shumsher also recognised the need for safe drinking water. Between 1866 and 1872, he had served as Nepal’s ambassador in Calcutta, and he must have seen water mains already in operation there, and a filtration plant inaugurated in 1870. Madras had installed such a system as early as 1800, Bombay constructed the Vihar and Tulsi reservoirs in the mid-19th century. In Kathmandu British Residency personalities such as George Gimlette must have urged Bir’s government to quicken the construction of the hospital and water system, yet the archival traces of such exchanges still await historical scrutiny. By the late 19th century, the British had developed a technological ecosystem for water supply, intakes, pipes, fittings, reservoirs, and trained engineers. Bir Shumsher appealed to the British Government in India for engineering assistance. A British engineer named Mr Feigneur surveyed Kathmandu to prepare maps, and estimated the volume of water that could be brought from the Rudramati River. In 1889, a more experienced engineer, Lockhart Matthew Sinclair arrived. He was a Scotsman educated at Wellington College and the Royal Indian Engineering College, with prior experience in constructing waterworks in Jubbulpore and the Viceregal Palace in Shimla. Appointed State Engineer of Nepal (1889–1892), Sinclair reviewed Feigneur’s plans, updated them, and chose the Bishnumati River as the source of the city’s drinking water. Sinclair’s design included a reservoir at Panipokhari, at 1,330m elevation and 30m above &nbsp;Tundikhel, thereby enabling gravity-fed distribution in pipes. With a capacity of 7,327 cubic metres, the reservoir could store nine days of supply.&nbsp; The system was designed to serve about 70,000 residents through both private connections and public standpipes. The reservoir was a single-compartment tank with an arched brick roof covered in earth and turf. Its brick walls were bonded with lime mortar and aggregate, and its floor was dressed with fly stone. Work on the valley’s water supply began in 1888, three years after Bir Shumsher seized power. The following year, Bir Hospital and the Bir Water Works took shape. The project involved some 40km of imported cast-iron pipes, weighing 1.866 million kg and inscribed with the marks of Scottish foundries ‘Ally and McLean’ and ‘Glasgow’. Construction required 620,000 man-days of labour and cost over Rs600,000. Transport costs inflated prices: <a href="https://commons-nepal.com/the-first-kaldhara-in-the-four-cities-of-the-valley/" target="_blank">a load of cement</a> costing Rs10 in Calcutta was worth Rs33 by the time it reached Kathmandu. Bir Water Works was inaugurated in September 1891, six years after the cholera epidemic. Water flowed out of 131 taps, including eight in Lainchaur, six in the royal palace, eleven in the prime minister’s palace, sixteen around Tundikhel, thirteen in Thapathali, seven in Thamel, and two in Naxal. The system’s designation, the term ‘works’ , echoes the Chelsea, Calcutta, and Glasgow Water Works, underlining its industrial pedigree. Water was also supplied to Phora Durbar, Bir Shumsher’s palace of music and dance whose fountains sprayed rose-scented water in a display of opulence. The <a href="https://commons-nepal.com/the-first-kaldhara-in-" target="_blank">Bir Dhara Works</a> was more than an engineering scheme: it was Nepal’s first modern public-health intervention. Safer drinking water curbed waterborne disease, and the number of cholera outbreaks declined, but were not eliminated.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260103020144_d5c22de54c0eaab680a166c5a7482839fdc09b60679109021d0504252a810254.png" data-media-id="editor_4" data-image-id="20260103020144_d5c22de54c0eaab680a166c5a7482839fdc09b60679109021d0504252a810254" data-rendition-name="original" width="865" height="535" loading="lazy" alt="Cholera and drinking water in Kathmandu"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260103020144_a46075b6d759585df56a2bb8e5a07d85de7d9a69406165c32784fe30012c9971.jpg" data-media-id="editor_5" data-image-id="20260103020144_a46075b6d759585df56a2bb8e5a07d85de7d9a69406165c32784fe30012c9971" data-rendition-name="original" width="2791" height="3859" loading="lazy" alt="Cholera and drinking water in Kathmandu"> </figure>  “Now we have water to fight cholera, and I believe cholera will no longer prevail. After four years of piped water, the benefits have been greater than expected,” Bir Shumsher said in a proclamation. Despite this, the prevalence of poor sanitation, open defecation, cramped housing, and malnutrition meant that typhoid, smallpox, and dyspepsia remained endemic. The Bir Dhara system marked Kathmandu’s transition from reliance on wells, rivers, springs, and hiti to piped water, operating for several decades and laying the foundation for the expansion of drinking water services across the country in the late twentieth century. <a href="https://commons-nepal.com/the-first-kaldhara-in-the-four-cities-of-the-valley/" target="_blank">Extensions followed in Patan</a> under Chandra Shumsher, and Bhim Shumsher later added the Tri Bhim Dhara. Piped water systems were subsequently constructed in towns such as Kirtipur, Bhaktapur, Dhankuta, Pokhara, Dhulikhel, and Jajarkot which itself saw a deadly cholera outbreak in 2009.&nbsp; CHOLERA METAPHOR In 1933, Nepal’s first water bureaucracy, the Pani Goswara, was established, formalising state involvement in urban water supply. Yet even till the late 20th century, households continue to rely on a mix of sources, including public water networks, private vendors, rooftop storage tanks, borewells, wells, hiti, and household filtration. The lack of reliable water supply places disproportionate financial, physical, and psychological burdens on low-income households, underscoring how decades of infrastructure expansion have not translated into universal, reliable service. during challenges in governance, investment priorities, and regulation. Bir Shumsher also attempted to introduce <a href="https://www.ukaalo.com/news/cholera-in-kathmandu-1958/" target="_blank">basic hygiene measures</a>, such as pit latrines with squatting slabs. However, there is no record of these facilities being built in his palaces, later built palaces, or elsewhere. Sanitation conditions remained poor for both the elite and the general population. Open defecation or the use of crude pit latrines without proper waste disposal was common. With no drainage or sewer systems, human waste accumulated near homes, contributing to the spread of waterborne diseases. In 2019, Nepal declared itself ‘open defecation free’, a policy milestone, but this achievement masks the persistence of deeper problems. Urban areas generate some 867 million litres of wastewater daily, yet only 7% of it is treated before being discharged. Sewage flows untreated into rivers and streams, spreading cholera, typhoid, dysentery, and other diseases, particularly among children and vulnerable communities. Safe disposal of faecal sludge continues to be a major struggle for many communities and local governments. Besides Jajarkot, Godavari in Kathmandu Valley had a localised outbreak in 2024. This year, Birganj was struck by a cholera outbreak caused by a lethal combination of unreliable water supply, groundwater overpumping, poor drainage and hygiene, and unsafe waste disposal. And Nepal’s peacekeepers deployed after the earthquake in Haiti in 2010 were blamed for spreading cholera that ultimately killed 30,000 people in the Caribbean nation. The Bir Water Works was more than a reservoir and pipes. It was Nepal’s first brush with modernity, mediated through engineering and haunted by cholera. More than 134 years on, cholera remains a threat and a reminder of Nepal’s challenges in water and sanitation governance. The issue is not merely ensuring access to safe water but also building public trust that quality essential services can be delivered equitably, sustainably, and with resilience. Ajaya Dixit is a Kathmandu-based researcher exploring Nepal’s water history since the mid-eighteenth century to inform ethical water and river management in a changing climate.

Life in a time of cholera

As someone born and raised in Patan, I knew that the city was rich in art, architecture and intangible heritage. But I never realised just how rich, and how little I knew about its hidden treasures until this book. Yala Mhasika/Exploring Lalitpur/Lalitpurko Chinari is published by the Lalitpur Chamber of Commerce &amp; Industry and introduces the city to the world, as well as to its own inhabitants. Lalitpur is popularly known as Patan, probably because of the pastures for livestock in its outskirts. Its original name in Nepal Bhasa is Yala, and is a blend of urban and rural, old and new.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_700fb4c7b27d78813f69347846403c492cd1d54e2f62e4ec097013714c4a2022.jpg" data-media-id="editor_0" data-image-id="20260101120152_700fb4c7b27d78813f69347846403c492cd1d54e2f62e4ec097013714c4a2022" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Patan Dhoka</figcaption> </figure>  Like other kingdoms in the valley of Swoniga, the dense urban cluster of houses, temples, monasteries were situated along the higher ground, while the farmlands were on the slopes leading to the rivers below. This unique townscape combined an urban lifestyle within a distinctly agriculture-based rural setting. The fertile soil, replenished by organic nutrients washed down from the streets above, as well as Kathmandu’s location on the ancient trade route between India and Tibet, provided the Valley’s kingdoms with prosperity – and thus the flourishing of art and culture over centuries. Most of Yala’s residents were farmers, traders, or artisans. Chinese visitors who came to Nepal in the 6th century saw that there were more traders than farmers, and more temples than houses. An entire street is inhabited by the descendants of Lhasa traders. Arniko is supposed to have been born in Yala.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_0fb490355fac9b8252c9abfbf5ef1bbac844b29103744a421eb6ef6dbc77dff7.jpg" data-media-id="editor_1" data-image-id="20260101120152_0fb490355fac9b8252c9abfbf5ef1bbac844b29103744a421eb6ef6dbc77dff7" data-rendition-name="original" width="2000" height="1332" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Kwonti area which houses five-storey Kumbeshwar temple dedicated to Shiva and Baglamukhi temple dedicated to Dasa Mahavidya shakti peeth.</figcaption> </figure>  Nepal exported goods and even minted coins for Tibet, and had a virtual monopoly of the major trans-Himalayan trade routes. This prosperity was reflected in monuments and shrines like the Kwa Baha Golden Temple. More so than the other three kingdoms of Swoniga, architecture flourished in Yala making it the centre for metal, stone and wood craft. The name Lalitpur means ‘city of fine art’ but with its sense of community, it might as well be a city of fine living. Legend also has it that the name Lalitpur comes from a farmer called Lalit who helped bring the rain god Karunamaya from Assam when the Valley was suffering a prolonged drought. Lalit’s shoulder beam stands to this day in Jhatapol. Disasters, invasion and <a href="https://nepalitimes.com/here-now/life-in-a-time-of-cholera">epidemics</a> were a recurring theme in Patan.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_b33b1024cb7a46f49fea35ecc9afa2740895907059d7a43c8bd6c463b1be05e7.jpg" data-media-id="editor_3" data-image-id="20260101120152_b33b1024cb7a46f49fea35ecc9afa2740895907059d7a43c8bd6c463b1be05e7" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Ajima of Haugal Tole which is the oldest stone scripture in Nepal with the Gaja Laxmi in Chyasal.</figcaption> </figure>  The book was put together by the heritage expert team of Rosha Bajracharya, Sunil Pandey and Anil Chitrakar and provides a socio-economic and political history of Patan – how it was always food surplus, thanks to sustainable farming until recently. Ground and drone images by Photo Venture Nepal in the book give us a rare new perspective on Patan. There is an entire chapter on the chariot festival of Karunamaya (Machhindranath), a community-managed festival with Barahi carpenters assembling the woodwork, vine engineers Yamva weaving rope and rattan for the 25m tall chariot, and Ghaku drivers controlling the speed and brakes as the structure rolls through narrow streets in the annual festival.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_d27b23aeb4548b0b64ab8ed20f40baa331060498c6b5443e2cb999b876c670af.jpg" data-media-id="editor_4" data-image-id="20260101120152_d27b23aeb4548b0b64ab8ed20f40baa331060498c6b5443e2cb999b876c670af" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Te Bahal in Patan which houses Karunamaya six months a year.</figcaption> </figure>  WALKING, WORSHIPPING The book can help in exploring Patan along five routes starting in Patan Dhoka, Pulchok, Shankhamul, Mahaboudha and Lagankhel with maps and details of the baha and bahil, shrines, ponds, open spaces, dhyochenn, courtyards and phalcha along the way. Because of its coffee-table size and heft, however, the guidebook is not practical to carry around. And despite detailed descriptions of the past and present of each site, readers are left wanting to know more about those places. It is proof of Patan’s vast treasures that even this book barely scratches the surface.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_31a597b7dc1bcc9f67b4f6a66b8c1c0e0a9406727389699e6aed9ac6c3c50901.jpg" data-media-id="editor_5" data-image-id="20260101120152_31a597b7dc1bcc9f67b4f6a66b8c1c0e0a9406727389699e6aed9ac6c3c50901" data-rendition-name="original" width="2000" height="1332" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Patukodom where visitors can view what remains of the ancient Kirant palace.</figcaption> </figure>  Some of the lesser-known must-visit sites include Patukodom which is all that remains of a palace of the original Kirat inhabitants of Patan. An archaeological dig here would surely unearth hitherto unknown facets of pre-Newa Patan. Then there are the slightly out of the way shrines like Mahabouha, a replica of a temple in Bodhgaya which houses 3,341 terracotta Buddhas with 90 big statues and which took 35 years and four generations to complete.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_ffb657dc254f707dc1755f6f13b1ef67bb7183b6573da9678c54482129fb3878.jpg" data-media-id="editor_6" data-image-id="20260101120152_ffb657dc254f707dc1755f6f13b1ef67bb7183b6573da9678c54482129fb3878" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Mahaboudha is a replica of a temple in Bodhgaya.</figcaption> </figure>  In a recent Patan by Night heritage walk, we learnt that Pim Bahal was the labour of love of a lakhe demon (now popularised as masked dancer) who had fallen for a local girl, and he dug the pond so she would not have to walk to a faraway spout to collect water. Nearby is the Charumati Chaitya, built by the daughter of Emperor Ashoka when she visited the Valley in the 3rd century BCE to spread Buddhism in Nepal. Interestingly, if Kathmandu is a city of temples, Patan is the centre of monasteries which represent a unique Tantric melding of Buddhist and Hindu forms. Examples are: the Tadham Cuka with relocated Licchavi-era chaityas symbolic of the four major events in Buddha’s life, Ajima of Haugal Tole which is the oldest stone scripture in Nepal with the Gaja Laxmi in Chyasal, and Bignantak Ganesa temple which is a manifestation of Shiva mingled with Vajrayana Buddhism.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_17a500e77f06b9881f684329e41d3482f6f6a639ffb929d8bb44e5af7934c61c.jpg" data-media-id="editor_7" data-image-id="20260101120152_17a500e77f06b9881f684329e41d3482f6f6a639ffb929d8bb44e5af7934c61c" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Bignantak Ganesa temple.</figcaption> </figure>  &nbsp;Besides spatial descriptions, the book also explains the temporal by curating a detailed cultural calendar of Lalitpur with dates and places of jatra, rituals, devotional dances and festivals that weave the agricultural cycle with the zodiac.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_b8e1cc03653fea85dec84a7abee4fd594c35c6ad553769f37905eb5b38774e08.jpg" data-media-id="editor_8" data-image-id="20260101120152_b8e1cc03653fea85dec84a7abee4fd594c35c6ad553769f37905eb5b38774e08" data-rendition-name="original" width="2000" height="1125" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Mipwa Lakhe of Patan which create fire in mid aid during performance.</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120152_442e10bff842214e8c7522ebf6e63663599768db73bb57d999deff9de1b59375.jpg" data-media-id="editor_9" data-image-id="20260101120152_442e10bff842214e8c7522ebf6e63663599768db73bb57d999deff9de1b59375" data-rendition-name="original" width="2000" height="1333" loading="lazy" alt="Exploring Lalitpur book review"> <figcaption>Gan pyakhan or Astamatrika dance which is performed in Patan Darbar Squre during Dasain. </figcaption> </figure>  The very last chapter is dedicated to water and nature, what sustains lives and civilisations, and how Lalitpur continues to be the city it is because of the water supply system our ancestors left behind which function still, despite encroachment and pollution. ‘In the history of the world cities have been built, they thrived for some time and then became archaeological sites because they were not able to maintain the quality of air, water, and its soil,’ the authors write. ‘This led these cities to depopulate and ultimately die and are only referred to in history books. Lalitpur is not going to make the same mistake.’ &nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260104080132_3f403388d57da82b499d6c489a8f095002bf69f11e515e92fa96fb5ca3af69e9.jpg" data-media-id="editor_10" data-image-id="20260104080132_3f403388d57da82b499d6c489a8f095002bf69f11e515e92fa96fb5ca3af69e9" data-rendition-name="original" width="1136" height="702" loading="lazy" alt="Exploring Lalitpur"> </figure>

YALA

For daring to demand democracy, the Rana regime hanged activist Shukra Raj Shastri at midnight on 24 January 1941 by the side of the road at Teku. Across town in Siphal, Dharma Bhakta Mathema was also hanged. Four days later, Dasrath Chand and Gangalal Shrestha were executed by firing squad. These four young revolutionaries were members of the underground Nepal Praja Parishad that led the anti-Rana revolution with plans to assassinate key figures of the dynasty. The four martyrs sacrificed their lives for an unfulfilled cause. Monuments were put up in their honour (Shahid Gate) and their names glorified by the Shah monarchy that itself went on to ban political parties and persecute democracy activists. In 1950, the newly-formed Nepal National Congress launched an armed uprising against Rana rule after King Tribhuvan sought refuge at the Indian embassy to flee from the Rana regime. In 1951, the Ranas, Nepali Congress and King Tribhuvan signed a tripartite agreement that brought an end to 104 years of Rana rule.&nbsp; Thus began contemporary Nepal’s cycles of unfinished revolutions. Some 75 years later, on a sunny September morning, Nepal’s young and hopeful took to the streets demanding an end to the nation’s corrupt polity, envisioning a better democracy. They organised through digital platforms, played songs, danced, and chanted slogans. A few hours later, commandos fired on the protesters, massacring dozens. Over 8 and 9 September 2025, the government was overthrown, constitutional bodies were literally reduced to ashes, and 74 Nepalis were martyred.&nbsp; Nepal’s periodic revolutions have been ignited by anger against rulers, they have begun with great promise, spread with enthusiastic popular support despite rulers trying to crush them — but ultimately they have always fallen short of the expectations of citizens demanding reform. Through decades of dissent, Nepal’s periodic revolutions have remained incomplete, with the nation caught up in a cyclical search for stability.&nbsp; In 1960, king Mahendra staged a coup and overthrew an elected government led by prime minister B P Koirala -- a royal revolution against democracy. Mahendra is reported to have famously said to Koirala: “Nepal is not big enough for the two of us.” For the next 30 years Nepal resembled a one-party state under the absolute monarchy of the Panchayat. Elected leaders languished in jail or exile, political parties were banned, and the press controlled. This was the most frigid period of the Cold War, with Nepal’s neighbours India and China at war. Geopolitics was bound to have an impact. “After the 1816 Sugauli Treaty with British India, external forces magnified internal power struggles as outsiders played divide and rule,” explains editor and political analyst Rajendra Dahal. “Movements did not reach a logical conclusion because domestic politicians were forced to compromise.” Indeed, the departure of the British from India in 1947 meant that the days of the Anglophile Rana regime were numbered. Successive prime ministers sought patronage in Delhi, and the monarchy tried to counterbalance it with a policy of equidistance with China. The neighbours showed a keen strategic interest in Nepal’s domestic politics. “The Panchayat system did not deliver what it promised,” says Santosh Sharma Poudel of Nepal Institute of Policy and Research. “Nepalis suffered administrative and governance failure, politics was centralised in Kathmandu, leaving out the rest of Nepal.” With mainstream political parties and leaders were &nbsp;underground between 1961 till 1990, student activists became proxies for political parties. As pressure for change grew, a student-led pro-democracy movement spread across Nepal in 1979. In response, King Birendra announced a referendum to allow Nepalis to choose between the status quo and a ‘reformed’ Panchayat &nbsp;system.&nbsp; The Panchayat won by a slim margin with questions about the legitimacy of the plebiscite. The reforms never materialised and it would be another decade before street anger boiled over again. As the People’s Movement for democracy spread, king Birendra again relented, unbanning political parties and Nepal became a constitutional monarchy. Inspired by Mao Zedong, a faction of Nepal’s Communists felt that western-style parliamentary democracy was too slow to end a feudalist monarchy. They launched an armed struggle in 1996, and the war lasted ten years (editorial, page 2). “If the democratic government post-1990 had performed better, and brought real reform, the Maoists would not have a reason to launch a revolution,” says Poudel. After nearly a decade of bloodshed that left 17,000 dead and thousands still missing, the Maoists joined forces with the democratic parties that they had been fighting, to pressure king Gyanendra through street protests in 2006 to restore democracy. In 2008, an elected Constituent Assembly abolished the monarchy. &nbsp;Recalls Rajendra Dahal: “The second people’s movement did not aim to abolish the monarchy. In fact, the reinstated parliament even granted equal rights for royal daughters to be crowned queen. But eventually, the monarchy no longer fit the political framework that the parties envisioned.” It took two elections over the next eight years to draft a new Constitution that reflected Nepal’s socio-cultural and geographic diversity and met the demands of the Maoists. The new federal Constitution was finally promulgated in 2015, but failed to satisfy India and the aspirations of the Madhes communities for autonomy. The state’s effort to crush the Madhes movement cost 45 lives. The promise of the new Constitution was squandered over the next decade with rotating leadership of the NC, UML and the Maoists — all of whom had forgotten the sacrifices made in the name of revolution. Cronyism and corruption was the order of the day. And it was this never-ending cycle of political opportunism and malgovernance that brought Nepal’s youth to the streets on 8 September.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120128_bc50f6370ff80a6758199ea7ba9f4c214656a9322a8d2ba1c97e6cdfb88f7f62.jpg" data-media-id="editor_0" data-image-id="20260101120128_bc50f6370ff80a6758199ea7ba9f4c214656a9322a8d2ba1c97e6cdfb88f7f62" data-rendition-name="original" width="3372" height="1371" loading="lazy" alt="timeline"> </figure>  1951 Revolution against the &nbsp;Rana regime 1960 King Mahendra's coup, jails B P Koirala and launches the partyless Panchayat system 1979 Student protests for democracy, King Birendra announces referendum&nbsp; 1980 Continuation of the partyless Panchayat system narrowly wins plebiscite&nbsp; 1990 People’s Movement I 1996 Maoists launch armed struggle&nbsp; 2000 Royal Massacre 2005 King Gyanendra's military-backed coup&nbsp; 2006 Comprehensive Peace Accord and Parliament restored 2008 Monarchy is abolished 2015 Madhes Movement, New Constitution promulgated 2017 First 3-tier election under federal system 2022 Second elections under federal Constitution&nbsp; 2025 GenZ protests BRK ALLIANCE “The socio-political change sought in all these movements never matched the people’s expectations, because the central issue of clean and efficient government never materialised,” says Poudel. The post-September political landscape has injected new personalities and alliances still relatively new to politics, as evidenced by the new electoral partnership of the BRK — Balen Shah, Rabi Lamichhane, and Kulman Ghising (page 1).&nbsp; These leaders are not without flaws, but they have become the effective flag-bearers of the GenZ movement, hoping to represent Nepalis disillusioned by decades of democratic decay. The March election will pit them against the legacy parties. There is already criticism that BRK is behaving just like male-dominated opportunists of old parties. The troika is resembling the triumvirate of Oli, Deuba and Dahal and its culture of patronage and quid-pro-quo power-sharing between alpha males. Will this also be another unfinished revolution? Says political scientist Sucheta Pyakuryal: &nbsp;“The kind of destruction that happened after the revolution should have been followed by a ground-breaking shift in Nepal’s political ecosystem, but that did not happen. Today the situation is a lot grimmer because we have players who have learned how to use the democratic facade to sound ‘equitable’ and ‘accountable’. But look closely and you see how the same political chauvinism, cronyism and nepotism still continue.”&nbsp;

Nepal’s incomplete revolutions

One of the few Newa towns situated outside Kathmandu Valley, Panauti still evokes the feeling of a place frozen in time.&nbsp; Largely untouched by haphazard urbanisation, this town 32km east of Kathmandu used to be a kingdom revered for the sacred confluence of the Punyamati and Rosi rivers.&nbsp; The Bramhayani temple is the site of a 12 yearly Makar Mela which is attended by devotees from as far away as India.&nbsp; Panauti’s crumbling monuments were restored in the 1990s by the French government. Temples, resting places, traditional homes were rebuilt and locals trained to revive their craft. Panauti and France marked 50 years of cooperation in September.&nbsp; However, the priceless murals on the temple walls are fading and need urgent restitution. Now, these crumbling wall paintings are meticulously documented in the Wall Paintings of Panauti and Their Context.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260106090116_31f6acf06ef879037fec8274b85153eab4468566abf71616490679bf8468b85d.jpg" data-media-id="editor_0" data-image-id="20260106090116_31f6acf06ef879037fec8274b85153eab4468566abf71616490679bf8468b85d" data-rendition-name="original" width="1596" height="1074" loading="lazy" alt="Panauti murals"> </figure>  In his foreword, French researcher Gérard Toffin writes about some of the earliest wall paintings from the Malla period in Kathmandu, including a 17th century mural depicting the procession of Rato Machhindranath which has since been restored.&nbsp; Several other pieces still exist but in a pitiful state, defaced by scratches. ‘They were painted on a plaster coating made of soil, husks, or limestone, which were applied to the bricks making up the walls,’ Toffin notes.&nbsp; The book delves into the cult of Asta Matrika among Newa of all castes and classes, the first of which is Bramhayani. These all-pervading deities are linked to Shaktism which focuses on the importance of the female principle and together, combine the forces of life, sex and fertility with that of death and eros. The deities are painted on the wall, carved on the stone or moulded into metallic statues.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260106090120_836efd2b0a569d8ec0fb2c6651a29b8f2dd8f8f75b72e27bb86b0bfc0ad8461f.jpg" data-media-id="editor_1" data-image-id="20260106090120_836efd2b0a569d8ec0fb2c6651a29b8f2dd8f8f75b72e27bb86b0bfc0ad8461f" data-rendition-name="original" width="1074" height="1434" loading="lazy" alt="Panauti murals"> </figure>  Riddhi Baba Pradhan, former director general of the Department of Archaeology who oversaw the restoration of Panauti 30 years ago, writes that a colourful wall painting depicting Buddha's past life at the Chabahil Chaitya built or restored during the reign of Lichhavi king Vrisdev in the 3rd century might be the earliest mural in Nepal. As for Panauti, a fragment from a 400-year-old scroll which illustrates a scene of Triveni Ghat with Dalinchok Hill in the background is likely the oldest. But that relic is currently at the Virginia Museum of Fine Arts in the United States.&nbsp; Pradhan recalls first encountering wall paintings inside Bramhayani temple which were deteriorated by smoke, leaky roof, dust, vermilion, sprinkles of animal blood and lack of maintenance. The team led by chemist Bhimvar Singh Thapa treated the wall paintings and some of the details were recovered including the paintings of Astamatrika and Asta Bhairav on the east, west and southern walls.&nbsp; PAINTINGS ARE NOT VISIBLE The murals were painted during the reign of the last Malla King of Bhaktapur Ranjit Malla and Queen Viswalaxmi Devi 300 years ago. But 40 years after the restoration, Pradhan notes that the murals are again in poor condition: ‘The paintings are not visible, the plaster is severely damaged and the surface has peeled off … electrical wires hang haphazardly inside the temple.’ The second lot of murals at Ghat Sattal are thought to have been commissioned during the late Malla period or the beginning of the Shah dynasty. Exterior walls depict incarnations of Lord Vishnu as well as Sesh Narayan, Ganesh, a scene of Samundra Manthan, of angels Maya, Moha, Ganga. Their attributes, dresses, ornaments, facial expressions, body postures are all skilfully represented but in a deteriorated condition.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260106090116_88d06703ae23a271905d81f35056d41df92cbbc4b9966fac3f34821659e585a8.jpg" data-media-id="editor_2" data-image-id="20260106090116_88d06703ae23a271905d81f35056d41df92cbbc4b9966fac3f34821659e585a8" data-rendition-name="original" width="588" height="862" loading="lazy" alt="Panauti murals "> </figure>  The wall paintings of Bramhayani Dyochhen are 90% degraded even though they were restored and repaired 40 years ago by the Panauti Integrated Project. Compared to other artefacts, wall paintings are more delicate to external factors, and if not preserved an important part of Nepal’s heritage will be lost.&nbsp; Furthermore, most of the wall paintings in Nepal are temperas, and not frescos. Tempera is painted with water-soluble mineral or vegetable pigments fixed with glue on the cow dung clay plaster on the brick walls. While Nepal’s focus has been on the repatriation of stolen artefacts from abroad, religious and cultural objects within the country like the Panauti murals need urgent attention.&nbsp; This slim publication by Panauti Municipality is an important call to begin the work before it is too late.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260101120124_d0efa1e57b2710a206beb37c7e934ac34e694afc278985934eac2fc52124a92c.jpg" data-media-id="editor_3" data-image-id="20260101120124_d0efa1e57b2710a206beb37c7e934ac34e694afc278985934eac2fc52124a92c" data-rendition-name="original" width="1136" height="702" loading="lazy" alt="Wall Paintings of Panauti"> </figure>

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