Swiss glaciers 1850–2100

Natural hazards

Less ice means new lakes, unstable slopes and thawing rock.

Retreating glaciers leave behind unstable moraines and new lakes, and remove the support from the valley flanks. Thawing permafrost loosens steep rock faces. Hazards appear in places that were long considered safe.

Monitoring has become essential: radar, GPS, satellites and cameras watch the most dangerous sites, and early warnings saved lives at Bondo, on the Weissmies and at Blatten.

Read about ice avalanches, lake outbursts and rockfall →

Sources

Sources

  1. Huss, Linsbauer & Naegeli (2025). Swiss Glaciers. State, projections and significance. Swiss Academies Factsheets 20(2). doi.org/10.5281/zenodo.14866776
Next: Life after ice →