A warming atmosphere also warms perennially frozen mountains. The stability of frozen rocks decreases with increasing temperature similar to how butter just taken out of a fridge &nbsp;becomes softer and less resistant to &nbsp;the cutting force of the knife. Thawing frozen mountains means softening them, making them less resistant against gravity, leading to breakage of small to large sections, resulting in rock falls, rock avalanches, and landslides. There is growing concern about <a href="https://nepalitimes.com/here-now/for-destruction-ice-is-also-great-and-will-suffice">the impact of global warming</a> on the stability of icy peaks in mountain ranges around the world, which several recent events in the Himalaya well illustrate. Permafrost is a technical short form of ‘permanent frost’ for frozen ground which remains at temperatures below zero degrees throughout the year.&nbsp; Permafrost is below the surface, is not directly visible, and therefore often escapes the attention of scientists and political authorities. Sophisticated methods must be used to explore it, such as drilling, geophysical soundings, or climate-related modelling.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_bbe43b730a10b861f318285a1999a1f6f4d245287618ff49ebfc8e51d154f573.jpg" data-media-id="editor_1" data-image-id="20240907160944_bbe43b730a10b861f318285a1999a1f6f4d245287618ff49ebfc8e51d154f573" data-rendition-name="original" width="4108" height="1000" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Even small glacial lakes, such as these currently forming near the terminus of the Kangchenjunga glacier in eastern Nepal, can be dangerous. Photo: ALTON C BYERS(Photo: Shristi Karki)</figcaption> </figure>  Generally, temperatures at surface level and directly below match the temperature of the air immediately above it. Polewards to around 60°N and S latitude, mean annual air and ground temperatures are mostly below 0°C. Permafrost is widespread in Alaska, northern Canada and Siberia. The lower limit of negative mean annual temperatures is at &nbsp;2,000-3,000m at mid-latitudes such as the <a href="https://nepalitimes.com/here-now/in-high-places">European Alps</a> or the Southern Alps of New Zealand, to 3,000-4,000m in the Himalaya, and to 5,000m near the equator in the Peruvian Cordilleras. Above these elevations, permafrost affects peaks. In high mountains the permafrost area is often far larger than their glacier-covered regions. In Nepal, the permafrost-affected area is about 2 to 3 times bigger than the glacier area, while in China with the perennially frozen Tibetan Plateau this factor is about 30. Temperatures decrease by 6-7°C for every 1,000m of altitude increase, and the coldest and most deeply frozen rocks are found in the highest parts of the peaks. The frozen zone inside mountains can reach depths of hundreds of metres. It is not just the ice on peaks in the European Alps or the Himalaya that is frozen throughout the year, but so are the rocks.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_b75f78e4ee6d146e797f06536491c445891fbeb578f60105f57247a8dc066bbd.jpg" data-media-id="editor_3" data-image-id="20240907160944_b75f78e4ee6d146e797f06536491c445891fbeb578f60105f57247a8dc066bbd" data-rendition-name="original" width="916" height="674" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Mt Chamlang (7,319m) with creeping frozen debris (rock glaciers, yellow arrows) and Lakes 464 and 465 (blue arrows) from glacier retreat at its foot. Mt Makalu (8,485m) is in the background.(Photo: Shristi Karki)</figcaption> </figure>  The sunny side of mountains are warmer, and the permafrost is thinner there than slopes in mountain shadow. Temperatures are not constant throughout the year, so a thin surface layer up to a few metres on top of permafrost that thaws in summer and freezes in winter. This seasonal freezing and thawing surface layer on permafrost is called the ‘active layer’. Deep, long-term freezing influences geomorphic processes inside mountains, drastically changing their properties. Growth of ice in cracks and fissures within solid rock tends to expand already existing openings, and even create new ones. The related weakening of bedrock, however, is compensated by strong adhesion and increasing strength induced by the ice fillings and related cold temperatures. Read also: <a href="https://nepalitimes.com/banner/tracing-past-glacial-floods-in-kangchenjunga">Tracing past glacial floods in Kangchenjunga</a>, Alton C Byers Not only the ice itself, but also rocks, rock-ice, and rock-rock contacts increase their strength with lower temperatures. Perhaps most important is the effect of freezing and ice filling of cracks between rocks containing water. Deep frozen rocks are essentially impermeable to water as an often-decisive factor of stability inside mountain slopes. In the abundant debris masses at the foot of high mountains, deep, long-term freezing causes even more spectacular changes. Formation of ice inside and beyond the pores can create a mixture of ice and debris with ice lenses, enabling such ice-rich frozen masses to slowly creep down the slopes of mountains. Landforms resulting from permafrost creep over past millennia look like lava streams and are called ‘rock glaciers’.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_dc86dc2e254de22afefcd3f6c2df76af6c0aab87555f702dc853992987dcb3fc.jpg" data-media-id="editor_5" data-image-id="20240907160944_dc86dc2e254de22afefcd3f6c2df76af6c0aab87555f702dc853992987dcb3fc" data-rendition-name="original" width="1072" height="625" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  Thawing out From long-term temperature measurements in deep boreholes, we know that global temperature increase of the atmosphere during the past about 100-150 years has warmed up mountain slopes down to depths below the surface of about 100m. The effect of this deep warming is the reversal of the freezing and cooling effects. It reduces the strength of rocks or debris with ice and makes them ‘softer’ and more permeable to water. Over the past decades, creep rates of frozen debris in rock glaciers have markedly increased, and the frequency of large rock-ice avalanches from high-mountain permafrost has accelerated. In the Peruvian Andes, two major events from mountain permafrost occurred in 2020 and 2023. Both had volumes of 1-1.5 million m3, reached lakes at the foot of the slope, and produced flood waves. The 2020 Salkantay flood caused loss of lives and heavy damage at Santa Teresa, 35km down valley. The flood wave at Rasac was fortunately retained within the lake at lower altitude. On 5 May 2012, a massive rock, ice, and debris avalanche from Annapurna IV <a href="https://nepalitimes.com/here-now/remembering-the-seti-disaster">cascaded into the Seti River gorge</a>, plummeting into a rockfall-dammed lake. The impact triggered an air blast that levelled thousands of hectares of forests, a dust cloud covered the countryside in fine white rock powder, and a hyper-concentrated slurry flood that killed 72 people downstream.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_81860cf5896090449c7fd074796f683c164e2bff782a46390cd43eee6202f19b.jpg" data-media-id="editor_7" data-image-id="20240907160944_81860cf5896090449c7fd074796f683c164e2bff782a46390cd43eee6202f19b" data-rendition-name="original" width="780" height="539" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Rock failure from Annapurna IV led to a series of cascading events that resulted in the Seti River flood of 2012 that killed 72 people. Map: J  KARGEL / D REGMI(Photo: Shristi Karki)</figcaption> </figure>  On 20 April 2017, a high altitude breakage of solid rock from the east face of Saldim Peak (6,388m) in the <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">Barun Valley turned into a 1.1 million m3 debris flow</a> of ice and sediment that plummeted 1,200m down to the Langmale Glacial lake below. Although the lake was less than 0.01km2 in size, the combination of lake water with melting ice from the ice-debris flow triggered a massive hyper-concentrated flood that destroyed forests, pastureland, and trekking lodges for several dozen kilometres to the Barun’s confluence with the Arun. In India’s Uttarakhand state bordering Nepal, the Chamoli event of 7 February 2021 was catalysed by the detachment of 20 to 30 million m3 of rocks and ice from a frozen, ice-clad peak. The ensuing avalanche developed into a rapidly flowing mass of rocks, ice and water, killing 204 people and heavily damaging an under-construction hydropower infrastructure 35km downstream.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_c7284846f8a571d8d1f5596b7731e7c4c2521f764aaf9e5df23ad9d0ad41d986.jpg" data-media-id="editor_9" data-image-id="20240907160944_c7284846f8a571d8d1f5596b7731e7c4c2521f764aaf9e5df23ad9d0ad41d986" data-rendition-name="original" width="798" height="462" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>This massive breakage (below) of solid rock from Saldim Peak in 2017 fell on a lake and unleashed a flood downstream on the Barun River. Top photo is of the peak before the collapse. Photos: ALTON C BYERS(Photo: Shristi Karki)</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_6e686f290b44e89cce8a1b822a74895c8d6a4ac4122572223ba3c4160b88879f.jpg" data-media-id="editor_10" data-image-id="20240907160944_6e686f290b44e89cce8a1b822a74895c8d6a4ac4122572223ba3c4160b88879f" data-rendition-name="original" width="799" height="470" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  On 3 October 2023, the collapse of about 15 million m3 of debris from a perennially frozen moraine into <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">South Lhonak Lake in the Sikkim</a> Himalaya produced a flood wave and debris flow which killed 14 people with over 100 missing, destroyed a hydropower reservoir at Chungthang, 60km downstream, and caused destruction of houses, roads, and agricultural land. Similar processes may have been involved in the Birendra Tal glacial lake flood of 21 April 2024 and <a href="https://nepalitimes.com/here-now/lives-on-the-line-in-the-himalaya">the Thame flood of 16 August 2024</a>. Each of the above cases show the potential hazard over long distances related to process chains, especially in connection with impacted mobile water bodies in glacial lakes and artificial reservoirs.&nbsp; <h2>12 TIPS: Awareness and Protective Measures</h2> Changes in high altitude permafrost, and the devastating geomorphic events they cause are still poorly understood by Nepal’s scientific community and government. Earthquakes and heavy rainfall are usually reported by the press to be the primary causes of catastrophic events, both of which are impossible to predict. However, climate change and gravity, the two major forces at work on Himalayan permafrost, are constants. As permafrost continues to destabilise at the highest altitudes in the Nepal Himalaya, more and more devastating events can be expected to occur.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_dd2d77fb090fb2f5c836411d61bd6e7bb4e2e40ea2abae3d8eee8a686e9457dc.jpg" data-media-id="editor_13" data-image-id="20240907160944_dd2d77fb090fb2f5c836411d61bd6e7bb4e2e40ea2abae3d8eee8a686e9457dc" data-rendition-name="original" width="977" height="733" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Gabions installed near Chukung in 2015 protected the village from a similar flood from the Lhotse Glacier in 2014. Photo: ALTON BYERS(Photo: Shristi Karki)</figcaption> </figure>  The question is, what can we do about it? Based on our collective experience in the European Alps, Peruvian Andes, and Nepal Himalaya over the past several decades, we offer the following suggestions: 1. Encourage more permafrost and hazard research. Nepal’s scientists and practitioners need to better understand and acknowledge the role of permafrost change in the growing list of climate change-related impacts in the high mountain environment, and more research of an applied nature is indicated. Interdisciplinary approaches that include and involve local people usually yield the most promising and effective results. 2. Standardise glacial lake risk assessment methods. Currently, scientists use various methods to assess a lake’s potential danger of flooding, with predictably mixed and widely differing results. Imja glacial lake in Khumbu, for example, is considered by some scientists to be extremely dangerous, and by others to have a low to moderate risk. The result is confusion among local people, local governments, and scientists alike. 3. Update and revise the current list of potentially dangerous glacial lakes in Nepal. The inventory should incorporate the changing permafrost factor, including smaller lakes less than 0.01km2. Even very small glacial lakes, such as those above Thame and the Langmale glacial lake in the Barun, can be as destructive as large lakes under the right conditions and cascading processes. 4. Develop new feasibility study protocols for large hydropower projects. These guidelines must incorporate the changing permafrost factor as well as the heightened threat of glacier floods. The potentially disastrous impacts of climate change upon major hydropower projects in Nepal have been predicted by scientists for decades, and yet the construction (and destruction) of major, multi-million-dollar installations continues. Hundreds of lives, and millions of dollars of infrastructure, stand to be saved through the use of more detailed, comprehensive evaluations of permafrost and glacier-related risks prior to project implementation. 5. Develop zoning policies. These should discourage the location of farms and infrastructure (homes, tourist lodges) within known and active floodplains. Some scientists believe that most of the deaths from the 2012 Seti flood could have been prevented had settlements not been located directly in the floodplain. 6. Simple is beautiful. Rock-filled wire cages (gabions) can be engineered to effectively divert floods and should continue to be promoted in high mountain regions. In the village of Chukung located directly in the floodplain of the Lhotse Glacier in the Sagarmatha National Park, for instance, the installation of gabions after a glacier flood in 2015 protected the village the following year when a second similar flood from the same glacier occurred.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_ce975f82275c7936c7948fbf7fd7231b61adecc01d5510760144a8f3d0467859.jpg" data-media-id="editor_14" data-image-id="20240907160944_ce975f82275c7936c7948fbf7fd7231b61adecc01d5510760144a8f3d0467859" data-rendition-name="original" width="1005" height="695" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  7. Build higher bridges. This can effectively address the growing frequency and magnitudes of glacier floods in the high mountains, eliminating the need for continuous rebuilding. 8. Increase awareness. Nepal’s mountains will continue to destabilise and become even more dangerous in future. Exercising extra caution while crossing a landslide, an active torrent, or a debris-covered glacier is a fact of life in today’s high Himalayan regions. Likewise, constructing a lodge, school, or community building beneath a small and seemingly harmless glacial lake should be discouraged. 9. Promote simple and effective early warning systems. In spite of their much-touted role in disaster mitigation, early warning systems installed to date at potentially dangerous glacial lakes in Nepal have proven to be expensive disappointments. They are typically installed by a remote and distant government agency, little training in their use by local villagers is offered, and local people say they have no idea what the warning sirens sound like nor what they should do if one goes off. Thus far the most effective and proven EWS tool has been the cell phone. Hundreds of lives were saved during the Seti River flood of 2012 when upstream witnesses phoned warnings to their downstream family and friends. 10. Improve mechanisms that allow scientists to communicate. The results of their permafrost and glacier hazard research should directly, quickly, and effectively be communicated to decision-makers. This has proven to be easy to recommend but difficult to implement in most of the world but is nevertheless in need of our constant efforts to achieve. 11. Encouraging transboundary permafrost research. Increased cooperation between scientists and researchers in Nepal, China, and India is needed to help identify potentially vulnerable crossborder rockfall, avalanche, and catastrophic flooding risk. 12. Develop and implement adaptation planning. Continue planning and training programs targeted at permafrost-related floods and other highland-lowland hazards. Local Adaptation Plans for Action (LAPA) have proven to be an effective tool for increasing local awareness of climate impacts as well as planning for mitigation measures. Dr Wilfried Haeberli is with the University of Zurich and Dr Alton C Byers University of Colorado at Boulder.

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The not-so-permanent frost

<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221110141128/636cfc6b9c7e80680e0a0b8ajpeg.jpg" alt="" width="2006" height="1332"/><figcaption>Paddy and maize fields in Kavre. A heavier than usual monsoon this year brought destructive floods, but was a boon to farmers. Photo: AMIT MACHAMASI</figcaption></figure>As if the <a href="https://www.nepalitimes.com/banner/first-drought-then-downpour/" target="_blank" rel="noopener noreferrer">drought</a>, <a href="https://www.nepalitimes.com/banner/wildfires-ravage-nepal-mountains/" target="_blank" rel="noopener noreferrer">wildfire</a> and <a href="https://www.nepalitimes.com/banner/disasters-in-nepal-come-in-waves/" target="_blank" rel="noopener noreferrer">flood disasters</a> this year were not bad enough, scientists have warned that unless the world reduces emissions of greenhouse gases drastically, these disasters will get much worse.Hundreds of scientists spent the past two years drafting a 4,000 page <a href="https://www.ipcc.ch/report/ar6/wg1/">report for the UN’s Intergovernmental Panel on Climate Change (IPCC),</a> but even as they did so, news of climate calamities were coming in thick and fast: <a href="https://www.nepalitimes.com/opinion/turning-on-the-heat/" target="_blank" rel="noopener noreferrer">heat waves</a>, continental-scale wildfires, flash-floods, biodiversity loss.A summary of the report for world governments was released on Monday, three months before world leaders meet in Glasgow in November for a Climate Summit called COP26 (Conference of Parties 26).The highly technical Sixth Assessment Report (AR6) of the IPCC on the science behind climate change has forecasts that will directly affect Nepal and the Himalaya. It also has pointers on what must be done urgently to reduce its impact.The IPCC report contains the most direct correlation scientists have drawn between <a href="https://www.nepalitimes.com/editorial/a-hotter-himalaya/" target="_blank" rel="noopener noreferrer">climate change and extreme weather</a> around the world.‘The frequency and intensity of heavy precipitation events … and droughts have increased since the 1950s,’ the report states with ‘high confidence’, adding that human-induced climate change is likely the main driver.It adds categorically: ‘Increases in monsoon precipitation since the 1980s have resulted from rising GHG (greenhouse gas) concentrations … Monsoon precipitation is projected to increase in the mid- to long term on a global scale, particularly over South and Southeast Asia.’<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221110141128/636cfc6e9c7e80680e0a0b8bjpeg.jpg" alt="" width="1988" height="1024"><figcaption>Source: IPCC</figcaption></figure>It predicts that these heavy precipitation events will intensify and become more frequent in most regions as the world continues to warm. Globally, there will be 7% more <a href="https://www.nepalitimes.com/editorial/climate-damage/" target="_blank" rel="noopener noreferrer">extreme weather</a> for every 1° Celsius of global warming.Even under the best-case scenario of reduced greenhouse gas emission, global average temperature is set to exceed 1.5°C by the turn of the century. <a href="https://www.nepalitimes.com/banner/a-biden-presidency-climate-and-the-himalaya/" target="_blank" rel="noopener noreferrer">The Himalaya</a> will get hotter faster than other parts of the world, and could warm by 1.8-2.2°C.The main conclusions of this IPCC report were leaked to AFP in June, and predicts global surface temperatures increasing until at least the mid-century even under the best scenario. The warming will ‘exceed 2°C during the 21st century unless deep reductions in CO2 and other greenhouse gas emissions occur in the coming decades’.The 2015 Paris Agreement recommended capping global warming at ‘well below 2°C’ above pre-industrial levels, and to 1.5°C in the next 30 years by reducing emissions. However, the increase is already at 1.2°C Celsius, and on track to exceed 2°C.This will lead to <a href="https://www.nepalitimes.com/banner/between-existence-and-extinction-in-nepal/" target="_blank" rel="noopener noreferrer">mass species extinction as ecosystems collapse</a>, more <a href="https://www.nepalitimes.com/banner/mosquitoes-move-up-mountains-as-the-earth-warms/" target="_blank" rel="noopener noreferrer">widespread diseases</a>, heatwaves making parts of the world unfit for human habitation, cities and small island nations at risk of being submerged by sea level rise.For Nepal, even a 1.5°C rise in global temperature will mean <a href="https://www.nepalitimes.com/editorial/manpower-and-hydropower/" target="_blank" rel="noopener noreferrer">heavy precipitation and associated flooding</a> of the kind the country saw in 2018 and this year. At 2°C increase, the floods, heat waves and droughts  will be even deadlier.The other impact on Nepal will be a <a href="https://www.nepalitimes.com/banner/on-thin-ice-in-the-khumbu/" target="_blank" rel="noopener noreferrer">Himalayan meltdown</a>, as the mountains thaw with rising temperatures.‘Human influence is very likely the main driver of the global retreat of glaciers since the 1990s,’ the report states. ‘…The global nature of <a href="https://www.nepalitimes.com/banner/human-face-of-a-himalayan-climate-crisis/" target="_blank" rel="noopener noreferrer">glacier retreat</a>, with almost all of the world’s glaciers retreating synchronously, since the 1950s, is unprecedented in at least the last 2,000 years.’<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221110141128/636cfc719c7e80680e0a0b8cjpeg.jpg" alt="" width="640" height="546"><figcaption>Future annual emissions of CO₂ under the five scenarios SSP1-1.9, SSP1-2.6, SSP2-4.5, SSP3-7.0 and SSP5-8.5. Source: IPCC</figcaption></figure>This is even truer for the Himalaya because of its proximity to the equator. Scientists say it is already warming up to 0.3-0.7°C faster than the global average due to a phenomenon called ‘Elevation Dependent Warming’. But at the current trajectory, the mountains may see warming of up to 5.7°C during this century. In such a scenario, the <a href="https://www.nepalitimes.com/banner/a-terrifying-assessment-of-himalayan-melting/" target="_blank" rel="noopener noreferrer">Himalaya will lose two-thirds of permanent ice</a>, and most glaciers will have melted.It predicts that even if greenhouse gas emissions are curtailed, <a href="https://www.nepalitimes.com/banner/the-third-pole-is-warming-faster-than-expected/" target="_blank" rel="noopener noreferrer">mountain and polar glaciers will continue melting</a> for decades or centuries. This will impact not just Nepal but about 1 billion people living downstream from the Himalaya in China, India, Bangladesh and southeast Asia.‘Human influence has likely increased the chance of compound extreme events since the 1950s, increases in the frequency of concurrent heatwaves and droughts on the global scale, fire weather in some regions of all inhabited continents, and compound flooding in some locations,’ the says the IPCC report, almost describing the winter drought, <a href="https://www.nepalitimes.com/here-now/weve-seen-fire-and-weve-seen-rain/" target="_blank" rel="noopener noreferrer">wildfires and floods that have ravaged Nepal</a> in the past 8 months.The main cause of all this warming is that in 2019, atmospheric CO2 concentrations were higher than at any time in at least 2 million years. Global surface temperature averaged over 2081–2100 will be higher by 1.0°C to 1.8°C compared to pre-industrial levels even if emissions are controlled in the next 30 years.The IPCC report summary says that the only solution is for world governments to immediately agree on reaching net zero anthropogenic CO2 emissions to stabilise human-induced <a href="https://www.nepalitimes.com/opinion/climate-for-change/the-great-himalayan-thaw/" target="_blank" rel="noopener noreferrer">global temperature increase</a>.If the biggest carbon emitters like India and China meet cut back targets, under the most optimistic scenario global average temperature would stabilise at below 1.5°C toward the end of the 21st century after overheating by 0.1°C. But experts do not sound very optimistic about this happening.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221110141128/636cfc749c7e80680e0a0b8djpeg.jpg" alt="" width="2006" height="986"><figcaption>Projected global temperature rise under the intermediate, high and very high GHG emission scenarios considered. Source: IPCC</figcaption></figure><a style="font-size: 15px; letter-spacing: 0.01em;" href="https://www.nepalitimes.com/banner/nepal-lockdown-proves-air-quality-can-be-improved/" target="_blank" rel="noopener noreferrer">Nepal’s greenhouse gas emission</a> is negligible, but it has doubled in the past seven years according to a mandatory report filed by the Ministry of Environment with the UN’s Framework Convention on Climate Change (UNFCCC). Most of this is because the volume of petroleum imports from India has doubled in the past 10 years to meet the demand of transportation, expansion of cement and other industries.Last year, Nepal had submitted its second Nationally Determined Contribution (NDC) to meet <a href="https://www.nepalitimes.com/banner/blueprint-for-a-net-zero-nepal/" target="_blank" rel="noopener noreferrer">zero emission by 2050</a>. Switching to electric public transport and battery vehicles to reduce the petroleum import bill by just 10% would save Rs21 billion a year. This will also clean up the air, dirty air killed 41,000 people in Nepal in 2019.It is a sign of just how desperate the situation is that the IPCC scientists say in their report that the only hope for life on the planet may be a major volcanic eruption this century that would reduce global surface temperature because the sun will be blocked out for 2-3 years.The reports says rather phlegmatically: ‘If such an eruption occurs, this would therefore temporarily and partially mask human-caused climate change.’

UN climate report declares planetary emergency

The RSP and its prime minister are being sworn in this week after gaining an unprecedented election victory. This is a welcome change for many Nepalis who see it as a remedy to decades of coalition instability.&nbsp; Yet Nepal’s political history suggests otherwise. No majority government has ever completed its full term. This reveals a deeper structural problem: weakly institutionalised parties dominated by personalities rather than ideas. 1951: Dissatisfaction with the oppressive Rana regime among the educated elite led to the creation of political parties like the Nepali Congress (NC), Praja Parishad (later merged into the Nepali Congress), Gorkha Parishad, and the Nepal Communist Party.&nbsp; They emerged secretly, mainly in India during the height of that country’s independence. They organised a successful armed uprising against the Rana rule.&nbsp; 1959: The NC won a two-thirds supermajority in the first general election. Within a year, King Mahendra staged a coup and established the partyless absolute monarchy called the Panchayat system.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260322130332_a416ab5703287898f0566dc6d2a6b95d797ce2f4ed55bffcfae2e8edc7737c5e.jpg" data-media-id="editor_0" data-image-id="20260322130332_a416ab5703287898f0566dc6d2a6b95d797ce2f4ed55bffcfae2e8edc7737c5e" data-rendition-name="original" width="675" height="849" loading="lazy" alt="Mahendra and BP"> </figure>  1991: After the People’s Movement, the ban on parties was lifted and Nepal became a constitutional monarchy. Elections were held under a new Constitution and the NC won 110 out of 205 seats, joining the United Leftist Front which functioned as a loose coalition.&nbsp; Prime Minister Girija Prasad Koirala’s first term ended with his resignation due to infighting, particularly with Ganesh Man Singh, who accused him of <a href="https://doi.org/10.2307/2645025" target="_blank">“emerging as a dictator, downgrading democratic norms and values, and even selling out national interests.”</a> Parliament was dissolved and the NC ended up losing the ensuing elections. 1994: Following the NC’s defeat, a <a href="https://doi.org/10.2307/2645025" target="_blank">hung parliament emerged</a> with the UML forming a minority government that lasted only nine months before collapsing after a no-confidence vote, allowing a NC-led coalition to return to power.&nbsp; 1999: Voters gave the NC a second chance and the party won 111 out of 205 seats. The party was divided between supporters of Koirala and Krishna Prasad Bhattarai, who became prime minister. &nbsp;The internal NC power struggle intensified and Koirala became prime minister again only to face bribery scandals, the Maoist insurgency, and the royal massacre.&nbsp; In 2001, under growing pressure from both the public and the party, <a href="https://www.nytimes.com/2001/07/20/world/nepal-premier-resigns-caught-in-chaos-after-royal-blood-bath.html" target="_blank">Koirala was forced to resign</a> to be replaced by Sher Bahadur Deuba. The party eventually split into Koirala’s NC and Deuba’s NC (Democratic). &nbsp;In this chaos, king Gyanendra dissolved the parliament and assumed executive powers.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260322130332_e107b95de5641044f72a13fd20f417d16b9a2d1ecbae3492126ee5fd4244bd84.jpg" data-media-id="editor_4" data-image-id="20260322130332_e107b95de5641044f72a13fd20f417d16b9a2d1ecbae3492126ee5fd4244bd84" data-rendition-name="original" width="1250" height="753" loading="lazy" alt="Deuba and Girija"> </figure>  2017: This was the first election under the federal constitution. The UML and Maoists created a surprise pre-electoral alliance, breaking the Maoist coalition with the NC. The left alliance won a massive victory with the UML winning 121 seats and the Maoists 53 seats. Prime Minister K P Oli fell out with Pushpa Kamal Dahal of the Maoists. The House was dissolved, with the UML itself breaking into factions. What followed was seven shaky coalition governments in eight years.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260322130352_8b09b374d7fcb811e0a652c7f60b30eea4b9052a19ed3d768ba8ca9aaeb4dec7.jpg" data-media-id="editor_5" data-image-id="20260322130352_8b09b374d7fcb811e0a652c7f60b30eea4b9052a19ed3d768ba8ca9aaeb4dec7" data-rendition-name="original" width="667" height="1000" loading="lazy" alt="Oli and Prachanda"> </figure>  2022: The RSP was formed only four months prior to elections, but managed to become the fourth-largest party. In this month’s &nbsp;election, the RSP won a commanding parliamentary majority by presenting itself to the electorate as different from the discredited old parties.&nbsp; The RSP leadership structure is largely personality-driven and opaque. Party leader Rabi Lamichhane joined the governing coalition with the Maoists and UML securing four ministerial positions. Lamichhane became Home Minister and Deputy Prime Minister, using his swing vote to be the kingmaker party in the coalition. Lamichhane was embroiled in various scandals which he blamed on political vendetta. There was internal dissent within the party and among supporters who felt the coalition betrayed RSP’s founding ideals.&nbsp; Lamichhane <a href="https://thediplomat.com/2023/02/key-ally-quits-government-in-nepal/" target="_blank">reportedly</a> bypassed the party’s internal mechanisms, unilaterally deciding to pull out of the government without broad consultation.&nbsp; The youth-led September protests gave the RSP an opportunity to represent GenZ aspirations, and its popularity was cemented after Balendra Shah joined the party as a prime ministerial candidate.&nbsp; With its dramatic election victory, there is a question whether the &nbsp;party can separate itself from its two leaders, and have internal democracy. Or will it just be a vessel for new political elites to continue staying in power?&nbsp; ‘BALEN PARTY’ The RSP has increasingly relied on the same tactics that the NC once used in its heyday. Backed by Balendra Shah’s meteoric rise to fame, the RSP is called ‘The Balen Party’. <a href="https://nepalitimes.com/opinion/cyberia/rsp-s-pr-list-is-not-good-pr" target="_blank">RSP’s PR list</a> includes celebrities, actors, singers, pageant winners, business personalities, and athletes to maximise visibility and public appeal. Many of these soon-to-be MPs have little to no experience working in government, or together as a team. Which is perhaps why they needed a two-day orientation last week. In today’s attention economy, political currency depends on visibility. This is why the RSP’s strategy to harness Shah’s popularity was necessary to secure victory, while Shah needed a political platform for the election.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260322130348_abd1522a1f4f8ad4a0861c3916d86bd9688deafc7c44081b976378405d2b8e39.jpg" data-media-id="editor_8" data-image-id="20260322130348_abd1522a1f4f8ad4a0861c3916d86bd9688deafc7c44081b976378405d2b8e39" data-rendition-name="original" width="900" height="900" loading="lazy" alt="Balen and Rabi"> </figure>  Political parties are essential for a democracy, but when they &nbsp;revolve around one dominant leader, internal institutions become weak, and decision-making becomes centralised in the leader rather than in party committees, rules, or ideological platforms.&nbsp; This is exactly what led to the downfall of the NC and the UML. Both over the years were ridden with inter- and intra-party strife and failed the electorate. RSP must take a lesson from this and unite to institutionalise beyond its two personalities. Or it will suffer the same fate as the legacy parties. Since its inception, RSP has espoused a populist and anti-establishment agenda. The ‘new’ RSP with the Balendra brand gained massive support by being a clear ‘other’.&nbsp; The RSP can fall into the same trap as the NC and the UML by defining itself by what it is not, rather than what it is for. Beyond the external enemies they oppose, these parties often struggle to articulate what they actually stand for.&nbsp; RSP positions itself as an alternative to established parties — a pragmatic, results-oriented political force rather than one driven by traditional ideologies. However,<a href="https://www.cambridge.org/core/books/abs/theorizing-in-comparative-politics/parties-and-ideology/8386083191B53EC86A239B8852D4A6A6" target="_blank"> ideology gives a party identity and direction.</a> Without ideological grounding, RSP risks becoming a hollow vessel for power-chasing politicians who oppose each other’s every move, a story that is all too familiar.&nbsp; RSP can no longer define itself as being anti-establishment. It is now the establishment.&nbsp; While RSP might look like Congress 2.0 to many who have seen Nepal’s democratic trajectory, RSP does differ from past majority parties in both positive and negative ways.&nbsp; Times have also changed. Nepal is no longer a monarchy, literacy rates are much higher, social media has made information more accessible, and Nepalis are less forgiving, as seen by the events that transpired on 8-9 September 2025.&nbsp; The RSP has fielded more qualified candidates, and they could steer the country in the right direction. Many are experts in their fields and have had years of experience prior to joining politics. Having experts from such different backgrounds is a huge asset.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260322130352_426011e8c377bffcef6fcb4371325b36fb940eb5a8ab66d3c76ff5cf6f1943c7.jpg" data-media-id="editor_10" data-image-id="20260322130352_426011e8c377bffcef6fcb4371325b36fb940eb5a8ab66d3c76ff5cf6f1943c7" data-rendition-name="original" width="1600" height="1066" loading="lazy" alt="RSP new MPs"> </figure>  Moreover, having MPs from various other parties/fields can also prevent a cult following of hardcore loyalists within the party.&nbsp; There are members loyal to certain RSP leaders in the party, but there are also those who will not hesitate to go against their leaders if need be. The RSP has little opposition in Parliament, so its own members may have to take on a check-and-balance role. Nepal is in a much better spot institutionally compared to what it was like back in the early days of its democracy. There is a Constitution, there is no active conflict, the monarchy is no longer an existential threat to democracy, and the local and provincial governmental bodies have had the time to settle.&nbsp; This means the RSP is in a better position to work without the basic institutional hurdles that previous governments faced, but it will not be able to hide behind institutional issues if it fails to deliver.&nbsp; In the past, majority parties could easily pin the blame on an authoritarian monarchy, a Maoist conflict, a lack of consensus during the constitution-building process, or a newly implemented federal system.&nbsp; Most of these were just excuses for incompetency. Governments were formed and fell based on self-serving negotiations, but they managed to keep the parties afloat, and the citizenry was willing to give them a second, third, or even fourth chance.&nbsp; The RSP will not have this privilege. Nepal has many problems, but its governmental bodies are better institutionalised than when the NC last had a majority. A challenge for RSP now would be fixing broken institutions, not building new ones. A recurring issue during Balendra Shah’s tenure as Kathmandu’s mayor were his <a href="https://kathmandupost.com/politics/2026/01/28/can-nepal-s-viral-mayor-run-the-country" target="_blank">disputes with the bureaucracy</a> that resulted in months of unpaid salary for KMC staff, a lack of collaboration between him and Deputy Mayor Sunita Dangol, and rarely any public appearances.&nbsp; The RSP is inheriting a bureaucracy tainted by deep-seated patronage networks. Sustaining a government requires institutional collaboration and a willingness to work together, not disruption and division.&nbsp; While Nepal has seen the rise of many populist figures in its democratic history, the RSP’s victory based on Balendra Shah’s fame is new. Populism is usually harmful for a democracy because it punishes dissent, turns criticism into betrayal, and fuels hyper-nationalism, authoritarianism, and polarisation. A trend of punishing criticism is already visible on online spaces. Without an effective parliamentary opposition, the responsibility for democratic accountability will fall on the media and civil society. If the trend of intolerance to criticism deepens, Nepal risks sliding toward a majoritarian politics where popularity replaces accountability. Time and again, the Nepali people have given opportunities to parties that promise change, only to face disappointment. Nepal’s political history shows that majority governments fail not because they lack seats, but because they lack institutions.&nbsp; The electoral earthquake Nepal just witnessed could bring sweeping reforms or drown the country’s fragile democracy. If RSP hopes to succeed where others failed, it must build a party that outlives its founders. Suvexa Pradhan Tuladhar is an Early Career Policy Research Fellow at the Nepal Institute for Policy Research (NIPoRe).

Will it be different this time in Nepal?

Next to my home in Bhainsepati stood a dead Uttis tree next to a public tap. A nearby water tank built a year earlier had killed its roots.
If the tree collapsed, people living nearby and those queuing up to fetch water at the tap would be hurt. With the storm season approaching, the risk was obvious. The tree could also fall on my own house, so I volunteered to find a way to remove this threat.
Little did I know how difficult it would be. A forest officer acquaintance told me there is a special procedure for cutting risky trees. I contacted the Lalitpur District Forest Office (DFO).&nbsp;
He said a technical report from a field officer was needed, and passed on her number. When I called, she asked for the location, photos, and a video. I send them all.
The ward office also suggested I use Lalitpur Metropolitan City’s mobile app, Lalitpur Alert, to report the problem. I uploaded photos, and submitted the complaint. This seemed to be very easy and efficient.
Indeed, the next day the municipality called me back and I explained the situation. They said they could not act without permission from the DFO. I asked why the app existed if the city could not act on such complaints. The officer said he did not know. My happiness was short-lived.
A couple of days later, the app notified me that my problem had been solved, and the complaint was removed. But the dead tree still stood there defiantly.&nbsp;
A week later, two forest technicians arrived on a scooter to inspect the tree. They looked up at the tree and asked if I had a measuring tape so they could measure its diameter.
“You are the technicians,” I told them. “You came to inspect the tree, and you came without a measuring tape?”
I rummaged at home and found a tape measure. They got the diameter and said they would prepare a technical report, but I would have to obtain a recommendation letter from the ward office and submit it to the DFO.
“This tree is dead,” I told them. “It is on public land. You have seen it with your own eyes. You know it's dangerous, so write a report and arrange for it to be cut. Why do I have to run from office to office to apply for recommendation letters?”
Their answer was simple, yet expected: “Those are the rules.”
They left, and I gave up. Two technicians spent half a day visiting the site. The metropolis runs a complaint system with a mobile app funded with public money. The ward office has staff to solve problems. Yet none of these institutions took the responsibility to remove a dangerous tree.
Everyone is busy citing rules and regulations and passing the buck. Weeks passed. Everyone reacted to the problem, but no one took any responsibility to resolving it.
Then, one bright December morning under a deep blue sky, a few neighbourhood boys were swinging their axes on the trunk. They had no proper equipment, no safety gear, and no professional experience.
I gave the boys some money and so did a neighbour. It took an hour or so for the tree to come crashing down safely. We had paid to have the tree cut illegally, and the matter ended there.
Multiple government offices, technicians, procedures, and mobile apps could not remove a dangerous tree, and we had to break the law to cut it. The tree is gone now, but the real problem remains: an inefficient bureaucracy.&nbsp;
It is perhaps symbolic that the tree is the election sign of the Nepali Congress, which was part of Nepal's governance and bureaucracy for decades and did not perform well in this month's election.&nbsp;
That is the bureaucracy that the new RSP government now has to get to work. But it will not be easy.
I posted on Facebook: ‘When people feel leaders have grown arrogant or corrupt with power, they change their minds and their votes. If those who replace them follow the same path, voters will again change their minds and votes.’
I continued: ‘The strength of democracy lies in this simple principle: the more citizens act as independent voters, the stronger democracy becomes. The more they behave as party loyalists, the weaker it grows. If we want a better system, we must demand deep reform of the state bureaucracy and hold institutions accountable.’&nbsp;
The first responses came from two senior government officials. They told me privately that they agreed by 200% but could not say so publicly.
It is quite normal for a Nepali to get the run around in government offices, it is almost a given to be asked for a bribe. As an environmental reporter and citizen, I have numerous such examples.
It is not just one sector that has been suffering. It is everywhere, and this is just an example of how complicated our bureaucracy is. As a 40 something person, I am old enough to remember the 1990 pro-democracy movement, &nbsp;the Maoist insurgency. Many promises made then by the politicians were broken.
We fought for rights, we fought for regime change. The country has changed political systems several times, from monarchy to multiparty democracy and finally a republic.
Yet one thing that remains largely untouched or reformed is our inefficient and corrupt bureaucracy. The new government, to be led by the youngest prime minister in our history must start this reform if it wants to deliver.&nbsp;
Otherwise, we may have to keep changing governments every few years, and still find ourselves unable to legally cut down even one dead tree.

A dead tree tests Nepal's bureaucracy

Sometimes, we need to take a step back to realise what a tectonic movement Nepali politics witnessed this month.
In a region and world ruled by elected authoritarians, Nepalis &nbsp;went to the ballot box freely to express a collective will for change.
These faces in this group photo of the RSP’s 180 freshly-minted MPs at the ballroom of the Royal Tulip Hotel on Wednesday is symbolic of what Nepal has come through.&nbsp;
The ship of state righted itself after the September Storm, installing an interim government that held an election within six months in which voters banished obsolete politicians and their parties into oblivion.
Nepalis, fed up with the inept kakistocracy of the past three decades, took the country into a post-ideological phase — replacing Marxists, Maoists and monarchists &nbsp;with a belief in a new governing culture that rewards delivery and accountability. And they have trusted the RSP to carry it through.
Nepal’s history has never been linear, it jerks ahead in lurches. The polity also tends to take one step forward and two steps back, so the public’s great expectations is tempered by a sense of cautious optimism and guarded pessimism.
This could be the great leap forward that Nepalis have waited for and deserve, but it could also be a Gramscian interregnum in which the old is dead and the new is not yet born. We will have to wait to see whether this transitional period will also see ‘morbid symptoms’.
As disruptor-in-chief, it was the Balendra Shah ‘wave’ or ‘craze’ that propelled the RSP to power. The former Kathmandu mayor needed a party platform, and the RSP’s tainted leader Rabi Lamichhane required a booster. Nepal's voters were looking for a saviour.
Personality-wise Shah and Lamichhane are poles apart: one is Type B and the other Type A. One is enigmatic, the other phlegmatic. But yin and yang do also tend to complement each other.&nbsp;
Kathmandu’s chattering class is already making self-fulfilling prophecies about the two falling out, and are fishing for hints that they already have. Shah’s absence from the RSP’s orientation this week was taken as a clue.&nbsp;
Closing the two-day tutorial on Wednesday, Lamichhane delivered a fiery 30-minute speech that laid out the RSP’s main agenda: to function differently from the old parties, serve the people, avoid middlemen, become true lawmakers without taking the law into their own hands.&nbsp;
“The old political parties contributed to history, we will build the future with a new political contract with citizens,” he said, trying to rise over past controversies and his abrasive rhetoric to sound statesmanlike.&nbsp;
GIVE AND TAKE
Lamichhane is said to be in touch with the reclusive Shah to announce a compact cabinet next week. Its composition will be an indication of how much give-and-take there was, and whether the criteria for selecting ministers is competence or loyalty.
Will RSP ministers behave like rulers or service providers? The new government will dive right into the economic fallout of the West Asia war with soaring fuel &nbsp;prices, inflation and uncertainty about remittance inflows.
On Thursday, Gagan Thapa resigned as NC chair, taking moral responsibility for the party’s election loss. The UML’s unrepentant K P Oli does not share the same sentiment about who is responsible for his own party’s historic downfall.&nbsp;
NCP chair Pushpa Kamal Dahal, who was luckier than his cross-party cohort, is now a comparative relic in a Parliament largely comprised of freshmen and sophomore lawmakers.
But the NC, UML and NCP still control provincial and most municipal governments. The old parties could try to make things difficult for the RSP at the centre, but it is also an opportunity for them to clean up their act ahead of local elections next year.&nbsp;
Another test for the RSP will be dealing with a heavily-politicised klepto-bureaucracy which has to frontend its policy decisions. &nbsp;

People’s power

Deadly floods two years ago along the southern fringes of Kathmandu Valley killed 200 people. Climate change was blamed, but the destruction was magnified by quarries and sand mining owned by local politicians and crony contractors. Disaster mitigation and environmental risk was not a priority for any of the political parties that ran and won Nepal’s election last week. Although the RSP has a supermajority, rural municipalities that grant mining contracts are still ruled by the established parties that supply aggregates and sand to feed &nbsp;Kathmandu’s construction boom. Here in Lele Valley, residents are worried about another monsoon season that will start in June and fear more floods bringing unmanaged gravel from quarries down the Nallu River.&nbsp; The house of Sanumaya Nagarkoti, 65, and ten neighbours were washed away by the flood on the night of 28 September 2024. She and her husband petitioned the ward and municipal council to remove the crushers but no one listened. The slopes above are scarred by landslides from two years ago, and the banks of the river are strewn with bounders the size of cars that were brought down. “We live in constant fear of landslides,” says Chakra Nagarkoti, “the heavy crusher machinery and tipper trucks also constantly shake the house.”&nbsp; Google Earth images show that 24.6 hectares of mountain flanks have been excavated since 2010, and despite the disaster no lessons have been learnt.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260319090348_bdce7f17500eadac0ce0814c32c2b4190d01325976fd4d29db9985148459c0bc.jpg" data-media-id="editor_0" data-image-id="20260319090348_bdce7f17500eadac0ce0814c32c2b4190d01325976fd4d29db9985148459c0bc" data-rendition-name="original" width="1500" height="907" loading="lazy" alt="Lele"> <figcaption>Photo: GOOGLE EARTH</figcaption> </figure>  The RSP might have got a near two-thirds majority in Parliament but decision-making at the community level is controlled by politicians in cahoots with contractors.&nbsp; Along the Mahadev Khola, the Department of Mines cancelled excavation permits for crushers citing flood and landslide risk. Yet there are still 21 contractors mining stones and sand.&nbsp; Nearby Godavari Municipality also instructed operators who had not renewed permits to close down. No action was taken. One of them is Vinayak Multipurpose which delivers aggregate and stones for United Cement. Local ward chair Milan Silwal, has a stake in Vinayak and locals accuse him of taking the side of industry.&nbsp; Another slope is being gouged out near Mahadev Khola, and comparing satellite imagery from 2010 shows that the scar on the mountain is now five times bigger.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260319090348_21a8f7f7f9d6cc784c35719da737b20283f934bbe16c9de971d91bf01012499a.jpg" data-media-id="editor_1" data-image-id="20260319090348_21a8f7f7f9d6cc784c35719da737b20283f934bbe16c9de971d91bf01012499a" data-rendition-name="original" width="1500" height="1125" loading="lazy" alt="Lele"> <figcaption>United Cement operating near Mahadev Khola. Photo: ARCHANA DARJI</figcaption> </figure>  Nearby stands the lone house of 55-year-old Sabina Tamang, who lives with her husband and daughter. Due to the sound of the stone-breakers, they cannot hear each other speak. “Last year, a landslide destroyed our cowshed and latrine,” she says. “Next it is going to be our home.”&nbsp; DRY SPRINGS Lele gets its water from several perennial springs which have gone dry in recent years. One of them is near where the cement factory quarries limestone. “We hardly get any water, and the little that does flow is murky and red,” says local resident Rajesh Shrestha. A parliamentary committee directive ordered excavation to stop 15 years ago after a similar flood to the one in 2024.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260319090352_af7da754299116578cc1dd91d5318ec337b69e74b0676599260b7c57c6ec6fd7.png" data-media-id="editor_2" data-image-id="20260319090352_af7da754299116578cc1dd91d5318ec337b69e74b0676599260b7c57c6ec6fd7" data-rendition-name="original" width="1440" height="494" loading="lazy" alt="Lele"> <figcaption>Lele over the years. Photo: GOOGLE EARTH</figcaption> </figure>  United Cement’s manager Hari Upreti says his company has fulfilled all requirements and has permission to mine 15 hectares of its own property and 4 hectares of government land. “We have the Department of Mines permit which is valid till 2036 and extract 1,600 tons of limestone every day,” says Upreti. “The local community knew about the mining and if there is a problem with springs going dry it is not because of us.” Environmental researcher Uttambabu Shrestha, however, says there is a direct correlation between the quarry operation and floods, landslides and dry springs.&nbsp; “Extraction should not be allowed without an environmental impact assessment, and companies must stick to set limits,” he says. Investigation of permits show that there is collusion between local officials and contractors. Godavari-6 Chair Bishnuman Maharjan has investment in two quarries and crusher companies operating along Nallu Khola. A paper trail links Maharjan also to Sagarmatha Stone Crusher and Mankamana Aggregate Industries. IMPUNITY&nbsp; Godavari Municipality published a notice in June 2024, instructing crusher companies to submit environmental reports within two weeks, covering initial examination and impact assessment. It also told them to pay local development fees and clear outstanding dues. The municipality even wrote to the Department of Mines clarifying that it had issued permits to only five out of 27 contractors. Within a month, the Department wrote to the District Administration Office (DAO) and District Police Office instructing them to stop illegal excavation, and sent a copy to the Lalitpur Division Forest Office. The DAO then wrote to Lalitpur Police naming Machindranath Multipurpose as operating illegally and should be shut down. There was no followup. The municipality then issued fines worth Rs 60 million to it and one other company for non-compliance. The companies stalled, disputing the calculations.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260319090356_6e96403d3c5be4aef4d030974d6d92029a0eb396deafd19c511978dae30dd3d2.jpg" data-media-id="editor_3" data-image-id="20260319090356_6e96403d3c5be4aef4d030974d6d92029a0eb396deafd19c511978dae30dd3d2" data-rendition-name="original" width="4000" height="2250" loading="lazy" alt="Lele"> <figcaption>Another site of extraction near Mahadev Khola in Godavari. </figcaption> </figure>  Machhindranath Multipurpose operator Kedar Timalsina Shashi denies doing anything wrong, and says the landslides were collateral damage because of the steep terrain. When contacted Godavari Municipality Deputy Mayor Muna Adhikari declined to comment. It has been 10 years since Rajesh Shrestha, Nikesh Shrestha, and others raised their voices against the environmental destruction caused by the construction mafia. An agreement was finally reached two years ago between locals and mining and transport businessmen, stipulating that stone mines must close permanently by mid-2025. The agreement also stated that check dams must be built to manage mining debris, and damaged structures must be restored to their original state. Trees were to be planted at sites where stone mines had operated. But the mines in the catchment are still in operation with 500 tipper trucks working on the site every day, transporting stones and aggregate. Local youth have continued holding sit-in street protests and at Lalitpur DAO.&nbsp; After one sit-in, the mines closed for about a month but they started back up a month later.&nbsp; Birendra Maharjan owns one of the crusher units, and says he follows all environmental protocols. He told us: “You need stones to build, and we must dig to extract stones. Some trees have to be cut, people get employment, and besides, floods and landslides happen across Nepal.” &nbsp;&nbsp; Centre for Investigative Journalism – Nepal.

permafrost

The not-so-permanent frost

UN climate report declares planetary emergency

Will it be different this time in Nepal?

A dead tree tests Nepal's bureaucracy

People’s power

Loot in Lele