Mountain erosion is not something new, but it seems to be happening much more frequently as the planet heats up and the permafrost that used to hold together high altitude peaks in the Alps and elsewhere in the world is no longer able to hold massive rock formations together.
On Wednesday, August 12, 2026, a major rockfall occurred on the north face of the Aiguille du Midi in the Mont Blanc massif above Chamonix, France. Over 500,000 cubic feet of rock broke away at an altitude above 11,800 feet (3,600 meters) in the Mallory area, sending a massive plume of dust and debris down the mountain.
This summer’s extreme heat waves destabilized high-altitude permafrost and rock walls, triggered safety checks by the Compagnie du Mont-Blanc and followed the closure of the peak's famous ice tunnel due to melting. Other iconic peaks are failing structurally too.
On the Matterhorn, intense summer heat waves have triggered frequent, erratic rock falls. Mountain guide associations in Switzerland and Italy have repeatedly been forced to suspend guided tours on major routes (like the Hörnligrat ridge) as the traditional frost holding the pathways together is simply liquefying.
Also, right now, scientists and residents are anxiously monitoring the Spitze Stei rock formation looming over the village of Kandersteg, Switzerland. Through decaying permafrost, the mountainside has been actively losing height and parts of it have been shifting by up to 70 centimeters (2.3 feet) per day during peak summer melt. Geologists estimate that if the unstable formation collapses all at once, it could unleash 500 to 700 million cubic feet of rock, creating a landslide that could dwarf the Blatten disaster of May 2025.
I guess that in the end, what goes up must always go down!






