Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3.5
Large, destructive avalanches have occurred naturally in the last 3 days. The most likely place to trigger one of these beasts is at upper elevations and on slopes that face NW-NE-S. Trigger points are where the weak layer is buried closer to the surface. Unfortunately, most of the time, it is impossible to identify those locations. Rocky outcroppings or wind-swept surfaces may give you clues about where those shallow areas are.
You are unlikely to notice obvious signs of instability, like collapsing or cracking, before triggering a slide. Snowpit tests may yield variable results, so rely on snowpack structure and recent avalanches when making decisions.
Your simplest and safest option is to avoid the problem by selecting low-angle slopes that are not connected to steep terrain. You are also less likely to trigger an avalanche on one of these weak layers where a hard and supportable crust exists just beneath the recent snow.
Overnight, the likelihood of natural avalanches will increase. Expect very large avalanches to fail naturally on these weak layers. Slides may run into lower elevations.
(3/8/2026)
A large natural slab avalanche on the slopes below the Little Matterhorn in the Avalanche Lake basin. This avalanche likely occurred when a smaller avalanche stepped down to a weak layer. The blue arrows indicate the crown of the thinner slab avalanche. Wind-drifted snow will continue to overload buried weak layers. Natural and human-triggered avalanches are possible on this layer.
Photo: Max Millington