Page 2: Research news on avalanche

An avalanche is a rapid, gravity-driven flow of snow, ice, and often entrained rock and debris that propagates downslope once the shear stress within a snowpack exceeds its shear strength. It emerges from mechanical instabilities in stratified snow layers, commonly at interfaces between weak layers and overlying cohesive slabs, triggered by loading, temperature gradients, or external perturbations. Avalanches can exhibit distinct flow regimes, including slab avalanches with brittle fracture and propagating crack fronts, loose-snow avalanches with point-release dynamics, and powder-snow avalanches characterized by turbulent, dilute suspensions. Their behavior is studied using snow mechanics, rheology, and fluid dynamics to model initiation, propagation, and runout.

Two Nepalis swept away by Annapurna avalanche

Nepali mountaineers on Tuesday searched for two people swept away by a powerful avalanche on the world's 10th highest mountain Annapurna, officials said.

Gliding avalanches: Field monitoring tackles the great unknowns

In a gliding avalanche, the entire snowpack slides down a suitable substratum such as grass or slabs of rock. Such avalanches are always released naturally. This requires the snow on the ground to become moist. In winter, ...

Physicists model how amorphous solids lose their stability

Why do avalanches start to slide? And what happens inside the "pile of snow?" If you ask yourself these questions, you are very close to a physical problem. This phenomenon not only occurs on mountain peaks and in snow masses, ...

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