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After Kalladi, Meppadi’s Biggest Fear Still Looms Above the Hill

A landslide at the Kalladi tunnel project has renewed fears in Meppadi, where residents say every monsoon brings uncertainty. Experts explain why fragile geology, changing rainfall and human interventions are increasing landslide risks.

Vaishnavi V S

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Excavated soil covered with blue tarpaulin at the Anakkampoyil–Kalladi tunnel construction site in Meppadi, Wayanad, where residents fear landslide risks during the monsoon.
A large mound of excavated soil covered with tarpaulins remains on the hillside above the Anakkampoyil–Kalladi twin-tunnel project in Meppadi, Wayanad. Residents say the slope has become a source of anxiety during every monsoon following the July 2026 Kalladi landslide. Photo: Vaishnavi VS/EdPublica

Every monsoon, residents of Kalladi in Wayanad look not at the rain, but at the hill above their homes. Two years after the Chooralmala tragedy, Kalladi landslide has reignited questions about whether fragile landscapes, climate change, and development are together creating an increasingly dangerous future.

MEPPADI (WAYANAD, KERALA): Every monsoon begins with a Look Up. When the rain begins, Nishal no longer watches the road outside his house. He watches the hill. A massive mound of excavated soil sits on the slope above his village in Kalladi, a hamlet in Meppadi panchayat in Kerala’s Wayanad district, where work on the Anakkampoyil–Kalladi–Meppadi twin-tunnel project is underway. It has sat there since the earth was excavated for the project, and with every spell of rain, it has become the first thing residents look at.

“People are scared to live here,” Nishal says. “The soil was kept there so it could be used later for construction. But once the monsoon arrives, we don’t feel safe anymore. If it isn’t managed properly, another disaster could happen.”

His fears are rooted in recent memory.

On July 7, 2026, a landslide swept through the tunnel construction site, killing eight workers. Although the disaster was far smaller than the Chooralmala-Mundakkai landslides that devastated Meppadi in July 2024, it reopened a question many thought would have been answered after that tragedy, two years ago: how safe are the hills people continue to live beneath?

A house stands below the Anakkampoyil–Kalladi tunnel construction site in Meppadi, Wayanad, where July 2026 landslide and stored excavated soil have heightened fears of future slope failures.
A house located below the Anakkampoyil–Kalladi–Meppadi twin-tunnel construction site in Kalladi, Wayanad. Residents living beneath the excavated hillside say every spell of monsoon rain renews fears of another landslide after the July 2026 disaster that claimed eight lives. Photo: Vaishnavi VS/EdPublica

The Landslide Changed the Questions

For Roshna, a former Block Panchayat member who lives near the construction site, the latest landslide has made every rainy day uncertain again.

“I am 56 now. If something happens to my house, I cannot build another one,” she says.

She is not opposed to the tunnel project. Few residents say they are. What worries them is whether the landscape has been made more fragile than it already was.

After the landslide, a committee was appointed to study how the excavated soil stored on the hill could be removed safely. Residents say experts have suggested reducing the height of the mound gradually instead of removing it all at once.

“I only want the issue to be handled properly,” Roshna says. “The project should be completed safely.”

More Than Just Heavy Rain

The Kalladi landslide has also drawn attention because it did not unfold under the same conditions as the Chooralmala disaster.

Scientific studies on the 2024 landslides show that Chooralmala was preceded by nearly two weeks of persistent rainfall that progressively saturated the slopes before they failed. That prolonged rainfall was a crucial factor behind the scale of the disaster.

Prof. S. Abhilash, Head of the Department of Atmospheric Sciences, Cochin University of Science and Technology say the situation at Kalladi was different.

“Landslides are not caused by the rainfall received on a single day,” he says. “What matters is antecedent rainfall. When rain continues over several days, the soil becomes saturated. At that stage, even another 20 or 30 millimetres of rain can trigger a landslide.”

That is why, he says, rainfall alone cannot explain the Kalladi incident. The geology of the slope and the way the landscape has been altered also need to be understood. He argues that replacing native deep-rooted trees with coffee and tea plantations, which have shallower root systems, has made the slopes more vulnerable to landslides.

Why Meppadi Keeps Failing

The hills around Meppadi have always been vulnerable.

The Western Ghats are among the oldest mountain systems in the world. Millions of years of weathering under the southwest monsoon have weakened the rocks beneath Wayanad. Above them lie thick layers of weathered soil. In places such as Meppadi, the terrain is further weakened by steep slopes, fractured rocks, foliated joints and geological lineaments.

“Meppadi has historically remained a landslide-prone area,” says Prof. S. Abhilash. “Not every high-hazard zone experiences repeated landslides, but this landscape has all the conditioning factors that make slope failure more likely.”

The record bears that out. In 2019, a landslide at Puthumala, another settlement within Meppadi panchayat, killed 17 people, five years before Chooralmala. Kalladi is now the third major landslide to strike this one panchayat in seven years. The Geological Survey of India estimates that nearly 19,301 sq. km, or 49.7 per cent of Kerala, falls within landslide-prone terrain, with Wayanad among the districts facing the highest risk — GSI assessments put 51 per cent of Wayanad and 74 per cent of Idukki on mountainous slopes classified as landslide-prone. Kerala recorded 2,239 major landslides between 2015 and 2022, the highest of any state in the country, according to Union government data.

A Changing Monsoon Meets an Old Landscape

The vulnerability of the hills is now intersecting with a changing climate.

Prof. Abhilash says the warming southeastern Arabian Sea is altering the behaviour of rain-bearing clouds over Kerala. Vertically developed cumulonimbus clouds that once discharged much of their moisture over the sea are increasingly moving inland. Over the past decade, northern Kerala has witnessed more frequent episodes of intense rainfall, contributing to flash floods and landslides.

But climate alone does not explain what is happening.

“The trigger may be rain,” he says, “but whether a slope fails depends on the condition of the landscape.”

Where Development Meets Risk

That is where residents believe the conversation should now shift.

Prof. Abhilash says replacing native forests with plantations, cutting roads through hillsides and excavating the base of slopes without adequate stabilisation can all increase landslide risk. In Kerala’s weathered mountains, where thick soil rests on fragile bedrock, even relatively small disturbances can destabilise a slope.

“The tunnel project is not the problem,” he says. “The question is whether the site was geologically suitable.”

He argues that infrastructure in fragile mountain regions should be preceded by detailed geological investigations, slope stability assessments and rigorous environmental impact studies rather than relying on engineering models developed for very different terrains.

Waiting for the Next Rain

After the Kalladi landslide, Dilip Buildcon Ltd — the construction company Konkan Railway Corporation awarded the tunnel project to in June 2025 — announced ₹6 lakh as immediate assistance to the families of its seven employees who died in the incident. The family of a contract worker was offered ₹5 lakh, while the Kerala government announced an ex gratia of ₹5 lakh for each bereaved family.

For Nishal and his neighbours, however, compensation is not what occupies their thoughts.

What they see every day is the mound of earth still overlooking their homes.

It is not simply excavated soil. It is a reminder that, in Meppadi, recovery is measured not only by rebuilding after a landslide, but by whether people can trust the hillside above them again.

Vaishnavi VS is an Editorial Associate at EdPublica. She holds a Master's degree in Mass Communication from Pondicherry University, India. She writes on education, science, environment, innovation, and public policy.

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Record Drought and Extreme Heat Push European Rivers to Lows as Wildfires Spread North

The European drought is driving rivers to record lows as extreme heat, wildfires, crop losses and water shortages put Europe’s energy and transport systems under pressure.

Sebin Pious

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European Drought: Rivers Fall as Heat and Wildfires Spread
The Rhine at Bonn-Limperich, Germany, during an exceptionally low water level, with the Konrad Adenauer Rhine Bridge and Siebengebirge (Seven Mountains) in the background. Image credit: Sir James/Wikimedia Commons, CC BY-SA 3.0.

A prolonged European drought combined with extreme heat is pushing major rivers to record lows, disrupting shipping and energy production while worsening crop losses and wildfire risks. As dry conditions spread north, Europe’s water, agriculture, ecosystems and public health systems are coming under increasing pressure.

A long period of low rainfall combined with extreme heatwaves has placed half of the European Union and the United Kingdom under drought conditions. A report published on August 12 by the European Commission Joint Research Centre and the European Drought Observatory reveals that nine percent of the region reached a critical alert level by late July.

Satellite data from Copernicus, the Earth monitoring program of the European Union, shows that severely dry soil is now damaging crops and plants across the continent. In its latest assessment, the observatory warned that “the drought has built up since early spring due to lower rainfall and higher than average temperatures, turning into fuel for devastating wildfires.”

European Drought: Rivers Fall as Heat and Wildfires Spread
Satellite imagery shows exceptionally low water levels along four of Europe’s major rivers—the Loire in France, Po in Italy, Rhine in Germany and Danube in Hungary—in early August 2026. Exposed sandbanks and riverbeds highlight the impact of prolonged drought. Image credit: European Union, Copernicus Sentinel-2 imagery.

European Drought Reaches Across the Continent

The lack of rain has driven four of Europe’s largest rivers—the Rhine, Danube, Loire, and Po—to dangerously low levels. Near Cologne, Germany, the Rhine fell to a fresh record low of 49 centimetres by mid-August, according to the Rhine Waterways and Shipping Authority — nearly 20 centimetres below the previous record of 68 centimetres set earlier in the summer, which had itself broken the prior all-time low recorded in 2018. Because large cargo boats need deeper water to float safely, operators have been forced to carry much lighter loads to avoid getting stuck on the riverbed, and in places river traffic has largely halted. Carrying smaller loads requires more trips, creating major shipping delays for important industrial materials across central Europe.

At the same time, low water levels and rising temperatures are creating a serious energy crisis across the continent. In France, power companies had to cut back nuclear energy production because river water became too warm to safely cool reactors without harming aquatic life. Hydroelectric power generation has also plunged across the Alps, northern Italy, and central-eastern Europe. Copernicus analysts noted that low river flows on the Danube are creating “serious operational challenges” for power plant cooling. In Italy’s Po Valley, the dried-out river basin has triggered a separate disaster: saltwater from the Adriatic Sea has flowed inland into depleted channels, ruining farmland soil and cutting off freshwater supplies for local crops.

Wildfires Burn Over 550,000 Hectares Across Europe

Dry plants and extreme heat have triggered widespread wildfires across the continent. According to August 11 data from the European Forest Fire Information System, 552,437 hectares of land have burned within the European Union since the start of the year, spread across 1,614 individual fires of 30 hectares or larger. Although this total remains below the 667,342 hectares burned by the same date in 2025 — a season that went on to become the worst on record for EU wildfires, with 1,034,552 hectares burned in total — it is significantly higher than the 20-year historical average.

Recent satellite data shows a clear shift: large wildfires are no longer staying just in southern hotspots like Spain and Greece. As dry weather pushes northward, fire risks are expanding into cooler regions, including northwestern France, southern Great Britain, the Alps, and the Balkans. Experts at the Joint Research Centre emphasized that “wildfire risk is no longer confined to southern Europe but is increasingly affecting wider parts of the continent under prolonged hot and dry conditions.”

Declining Harvests and Rising Health Risks

Continued heat and dry soil are dealing a heavy blow to European farmers. According to assessments by the European Joint Research Centre, crop yields across central and eastern Europe have dropped significantly. Production estimates for key spring and summer crops, such as grain maize and sunflowers, have fallen by six to seven percent. Winter crops have also suffered, with yield forecasts declining between one and four percent compared to earlier projections.

High temperatures are having a severe impact on human health as well. Monitoring data from public health agencies and the World Health Organization reveals a sharp surge in heat-related emergency admissions and deaths during extreme temperature episodes. Data compiled from national health agencies — including Germany’s Robert Koch Institute, which alone recorded an estimated 11,900 heat-linked deaths — put the region’s heat-related death toll above 25,000 as of early August, highlighting the severe human cost of this summer’s weather.

Seasonal Outlook and Emergency Response

Weather predictions indicate that dry conditions will continue through early autumn. According to the Copernicus Climate Change Service, drier and warmer weather is expected to persist across central-western Europe and southern Scandinavia through September. Climate experts also warn that a developing El Nino pattern could keep global temperatures higher than normal well into spring 2027. “Water resources, crops, energy systems, river transport, and ecosystems are all under growing pressure,” the report warned, with heatwave risks remaining high through August.

To coordinate emergency aid, the European Union activated its Civil Protection Mechanism. A dedicated fleet of 22 firefighting aircraft, 5 helicopters, and ground teams have been placed on standby across 12 countries. Meanwhile, the Copernicus satellite service has responded to more than 30 emergency requests since June, providing real-time mapping data to help local authorities track active fires and assess land damage on the ground.

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Indigenous Peoples and Nature Conservation: What the Research Shows

Research shows that Indigenous Peoples and local communities play a significant role in protecting forests, biodiversity and carbon-rich ecosystems. Evidence suggests that secure land rights, traditional ecological knowledge and equitable participation in conservation governance can strengthen environmental outcomes.

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Indigenous women standing beside a large tree in a tropical forest, illustrating the relationship between Indigenous communities and nature conservation
Indigenous women stand beside a large tree in a forest, reflecting the connection between Indigenous communities, traditional knowledge and the ecosystems they help manage. Representational image. Image credit: Bill Salazar/Pexels

Climate and biodiversity policies often focus on forests protected, carbon stored and species conserved. But an increasing body of research points to another factor that can influence these outcomes: who lives in, manages and makes decisions about ecologically important landscapes.

There are an estimated 476 million Indigenous Peoples across 90 countries, representing about 6.2% of the global population. Their territories overlap with many of the world’s remaining ecologically important landscapes, making their role increasingly relevant to climate and biodiversity policy.

The evidence does not support the blanket claim that Indigenous Peoples are inherently better conservationists. It does, however, show that land rights, ecological knowledge and meaningful participation in environmental governance can be important to conservation outcomes.

Indigenous Lands Overlap With Important Ecosystems

A 2018 study published in Nature Sustainability mapped Indigenous lands across 87 countries and politically distinct areas. It estimated that Indigenous Peoples manage or have tenure rights over at least 38 million sq km, more than one-quarter of the world’s terrestrial surface.

Their territories intersect approximately 40% of terrestrial protected areas and ecologically intact landscapes, including boreal and tropical primary forests, savannas and marshes.

The finding does not mean all Indigenous territories are pristine or formally protected. It demonstrates the substantial geographical overlap between Indigenous lands and landscapes that remain important for conservation.

That overlap matters for climate policy as well. Forests, wetlands and other intact ecosystems store carbon while supporting biodiversity and regulating water and other ecological processes.

One-third of Irrecoverable Carbon

The climate significance becomes clearer when carbon is considered.

A 2022 study in Nature Sustainability identified 139.1 gigatonnes of irrecoverable carbon remaining in Earth’s ecosystems, with considerable uncertainty around the estimate. The researchers found that 33.6% of this carbon—46.7 gigatonnes—is within lands managed by Indigenous Peoples and local communities, compared with 23% within protected areas.

“Irrecoverable” carbon refers to ecosystem carbon that, if released, could not be restored by mid-century—the timeframe considered critical for reaching net-zero emissions.

The figure does not mean Indigenous management itself creates these carbon stocks. It shows that a substantial share of carbon that climate policy has strong reason to protect is located within Indigenous and local-community lands.

Knowledge Accumulated Through Generations

Indigenous knowledge adds another dimension. Indigenous and local communities have developed detailed knowledge of species, habitats, seasonal cycles and natural resources through long-term relationships with particular landscapes. Such knowledge can complement scientific monitoring, particularly when environmental changes are observed over long periods.

The important question, however, is not simply whether conservation projects can use this knowledge. It is whether the people who hold it have a meaningful role in decisions affecting their territories.

A 2024 review in One Earth examined this question across conservation research. The researchers reviewed 648 empirical studies and analysed ecological outcomes in a subset of 170 studies. They found that more equitable governance arrangements—where Indigenous Peoples and local communities had equal partnership or primary control—were associated with significantly more positive ecological outcomes.

The study identifies an association, not proof that Indigenous governance automatically produces better results in every ecosystem. Conservation outcomes also depend on local institutions, ecological conditions, economic pressures and enforcement. But the finding challenges a model in which communities are merely consulted after conservation decisions have already been made.

The 30% Target Makes Governance Important

This issue is becoming more relevant as countries work towards the Kunming-Montreal Global Biodiversity Framework’s 30-by-30 target: conserving and effectively managing at least 30% of terrestrial, inland-water, coastal and marine areas by 2030.

The target itself calls for conservation areas to be equitably governed and recognises the rights of Indigenous Peoples and local communities where applicable. That means expanding protected areas cannot be measured only in hectares. How those areas are governed—and who has authority within them—also matters.

Climate Action Can Create New Pressures

The relationship between Indigenous territories and climate policy is not limited to forest conservation. The transition away from fossil fuels requires minerals used in batteries, electricity infrastructure and other technologies. Research published in Nature Sustainability found that more than half of the world’s energy-transition mineral resource base is located on or near the lands of Indigenous and peasant peoples.

This creates a potential contradiction: technologies intended to reduce emissions can generate new pressures on land and communities through mineral extraction.

A credible climate transition therefore has to consider not only the emissions avoided by new technologies, but also where their materials come from and whose territories are affected.

India: Where Forest Rights Meet Conservation

The global evidence has a clear relevance to India, although India’s legal framework generally uses the terms Scheduled Tribes and other traditional forest dwellers rather than the broader international category of Indigenous Peoples. India’s 2011 Census recorded about 104 million Scheduled Tribe people, representing 8.6% of the country’s population.

Forest-dwelling woman in traditional attire collecting resources from a stream, reflecting Indigenous and tribal communities’ relationship with forests in India
A forest-dwelling woman gathers resources from a stream, illustrating the close relationship between India’s tribal communities, forests and natural resources. Representational image. Image credit: masudar rahman/Pexels

The Scheduled Tribes and Other Traditional Forest Dwellers (Recognition of Forest Rights) Act, 2006, commonly known as the Forest Rights Act, recognises rights of forest-dwelling Scheduled Tribes and other traditional forest dwellers over forest resources. It also provides for community forest-resource rights, including the right to protect, regenerate, conserve and manage community forest resources. Government data show the continuing scale of implementation.

As of December 31, 2025, the Ministry of Tribal Affairs reported 44,33,940 forest-rights claims had been settled, meaning a decision had been taken. These comprised 42,56,845 individual claims and 1,77,095 community claims. The data cover implementation in 20 states and one Union Territory.

The difference between individual and community claims is significant because community forest rights concern collective relationships with forests and their management. For India, therefore, the conservation question is not simply how much forest can be protected. It is also how communities with established relationships with forests participate in managing them and how their legally recognised rights are implemented.

What the Evidence Tells Us

The research does not justify portraying Indigenous Peoples as universally or inherently sustainable. Their communities, institutions and environmental practices differ widely. The evidence supports a more precise conclusion.

Indigenous Peoples manage or have tenure rights over at least 38 million sq km in the countries covered by the major global mapping study. Their territories intersect about 40% of terrestrial protected areas and ecologically intact landscapes. Indigenous Peoples and local communities manage lands containing 33.6% of the world’s mapped irrecoverable carbon. And a review of 648 conservation studies found that more equitable governance was associated with more positive ecological outcomes.

Together, these findings suggest that Indigenous Peoples should not be viewed simply as beneficiaries of conservation programmes or sources of traditional knowledge. They are already part of the governance of many ecologically important landscapes.

For climate and biodiversity policy, the implication is straightforward: protecting ecosystems can also require protecting the rights, knowledge and decision-making roles of the people who live with them. While that does not replace scientific research or environmental regulation. It expands the evidence and the institutions available to protect nature.

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From Fighting Water to Saving It: The Netherlands Faces a Growing Drought Challenge

A land built to keep water out is now struggling to keep enough of it in — forcing a world leader in water management to rethink its infrastructure

Sebin Pious

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Netherlands drought challenge
Low water levels on the Nederrijn near Arnhem's Andrej Sacharovbrug, 5 August 2026. Photo: Tomas Guus / Wikimedia Commons (CC0)

The Netherlands built its global reputation by keeping water out. Now, longer dry spells and intensifying heatwaves are forcing the country to confront a very different problem: how to keep enough fresh water in the landscape. From greenhouse agriculture to homes built on wooden foundation piles, the Netherlands drought challenge is exposing the limits of infrastructure designed primarily for flood protection.

When people think of the Netherlands, the images that come to mind are windmills, tulip fields and the great sea walls that have kept the ocean at bay for centuries. The Dutch built their reputation, and much of their nation, on mastering water — pumping it away, holding it back, and reclaiming land from the sea to build a prosperous country on ground that, by rights, shouldn’t exist. Yet beneath that carefully engineered landscape, the Netherlands is now facing an unfamiliar problem: it is running out of fresh water.

As repeated summer heatwaves sweep across Western Europe, Dutch water authorities say they have reached the limit of what engineering can do. In several regions, officials have exhausted every standard measure available to them and are left with what amounts to a last resort — waiting, and hoping, for rain.

Netherlands Drought Challenge: From Floods to Water Scarcity

To understand how a country famous for its rainfall and rivers has arrived at this point, it helps to look at how the land itself was designed. For generations, the Dutch water system had one job: get excess water out to sea as fast as possible, to prevent flooding. That same efficiency has become a liability as weather patterns shift towards longer dry spells and more intense heat. The pressure peaks in late summer, when temperatures regularly cross 35°C and water evaporates faster than rainfall can replace it.

The consequences of shrinking water reserves go well beyond the daily weather report. They are already reaching into the economy, and into the foundations — quite literally — of Dutch homes.

Thousands of historic Dutch houses stand on wooden foundation piles. When groundwater levels drop, those piles are exposed to air and begin to rot. On clay and peat soils, the ground shrinks unevenly, pulling foundations down and cracking brick walls

Economic Strain and Sinking Homes

In Westland, the heart of Dutch greenhouse horticulture, the Delfland water authority has banned growers from drawing irrigation water from local ditches and canals — the first such ban in its history. According to the growers’ umbrella body Glastuinbouw Nederland, the ban affects around 150 commercial growers, with potential damages running as high as €150 million.

At the same time, a quieter crisis is unfolding beneath people’s homes. Thousands of historic Dutch houses stand on wooden foundation piles. When groundwater levels drop, those piles are exposed to air and begin to rot. On clay and peat soils, the ground shrinks unevenly, pulling foundations down and cracking brick walls. The Council for the Living Environment and Infrastructure estimates that close to half a million buildings across the country could show foundation damage by 2035, with repair costs reaching as much as €54 billion.

From Water Battle to Water Sponge

This reality is forcing a fundamental shift in how the Netherlands manages its resources. For centuries, Dutch policy was simple: fight the water, and push it away. Today, water authorities are engaged in a delicate balancing act, trying to save every drop using canal locks and storage basins. But holding onto existing water can only do so much once the rain stops altogether.

Long-term resilience will require redesigning the landscape itself. Rather than treating rainwater as a threat to be flushed out to sea, experts increasingly argue that the Netherlands needs to function more like a giant sponge — capturing heavy winter rain and storing it safely to survive the dry summer months that are becoming the norm.

A Lesson Beyond Borders

What is unfolding in the Netherlands carries a lesson well beyond it. If a nation this experienced in water engineering is struggling to keep pace with a changing climate, it says something about how quickly conditions can outrun even the most sophisticated infrastructure. As riverbeds stay low and the dry spells drag on, the Dutch find themselves in an unfamiliar position for a country built on water: waiting for the skies to open.

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