
Recent rock-ice avalanches and landslides in Nepal point to destabilised high mountains.
Repeated rock-ice avalanches and landslides in Nepal, including a recent event in the Gorkha district, have devastated rivers and infrastructure, leaving experts pointing to climate-driven mountain destabilisation.
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Repeated rock-ice avalanches and landslides have struck Nepal's high mountain regions, destroying infrastructure and causing massive casualties earlier in the year.
The rock-ice avalanche near the Nepal-Tibet border that opened the floodgates in the Bhotekoshi and Trishuli rivers on August 26 killed more than 1,450 people, with nearly 6,000 others still missing. It was followed by a massive landslide after parts of a mountain collapsed into a river in the Mustang region in late September.
And on Sunday, another rock-ice avalanche flooded the Budhi Gandaki River – which joins the Trishuli downstream – in central Nepal’s Gorkha district, with concrete-like slush swallowing houses, bridges and trekking trails, though no casualties were reported.
“To have two similar events, nearby and in one year, is unprecedented in Nepal,” said John Pomeroy, director of the Centre for Hydrology at Canada’s University of Saskatchewan, who has been following the events.
“While climate change did not directly trigger these catastrophes, the thawing of frozen ground, melt of glaciers, increased lubrication of frozen materials from rapid snowmelt and rainfall all destabilised the high mountains and created the preconditions that permitted these events to form.”

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The Central Meteorological Observatory predicts that in the next 10 days, the cumulative precipitation will be 10 to 30 millimeters in the eastern part of Northwest China and central and northern North China, 50 to 80 millimeters in the middle and lower reaches of the Yangtze River, and more than 200 millimeters in some places such as northeastern Sichuan; cold weather The air activity is frequent, and the average temperature in Xinjiang, North China and other places has turned 1 to 2°C lower, and it has been higher in the south of the Yangtze River and in the south of China. There was a significant cooling process on the 15th-18th, 20-21st, and 23-24th, with local rain, snow or sleet.