From Alaska's fjords to the Himalayas, a warming cryosphere is triggering floods, landslides and waves that science long predicted but politics ignored.
In August 2025, a landslide in an Alaskan fjord sent a 500-metre-high wave surging through waters regularly crossed by cruise ships. Weeks earlier, a collapsing glacier in Switzerland's Valais canton had buried most of the village of Blatten under a torrent of debris, despite an evacuation order that saved most of its residents. Neither event was a freak accident. Both were expressions of a single, measurable process: the rapid disintegration of the planet's frozen water under sustained global heating.
The cryosphere — the collective term for all of Earth's ice, snow and permafrost — is retreating at a pace that is destabilising the ground itself. As glaciers pull back, they leave behind slopes of loose, unsupported rock that are highly vulnerable to collapse. Permafrost, which has long acted as a kind of natural cement binding mountain faces together, is thawing as freezing levels rise, turning solid cliffs into unstable masses. Glacial meltwater fills hollows and depressions, creating lakes that can breach without warning and funnel enormous volumes of water into inhabited valleys below.
In Uttarakhand, India, a comparable deluge in 2021 destroyed two hydroelectric plants and killed around 200 people. Alaska illustrates another dimension of the problem. The loss of vast ice sheets has reduced the pressure load on the crust beneath, allowing the land to rebound and, in some models, increasing volcanic and seismic sensitivity over geological timescales. The geosphere — the rocky body of the planet — is not as separate from the climate system as was once assumed.