Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 2
Upper elevation terrain is the most likely place to find and trigger wind drifts that formed over the past few days. The weak layer would the loose, dry snow that was on the upper elevation, shady slopes before Thursday’s snow. The slab is a combination of various wind slabs and the new snow.
Approach steep, upper elevation shady slopes with caution - this is where slab avalanches can be triggered today, possibly remotely or breaking out above you when you’re part way down a slope. Small soft slabs and loose sluffs can be triggered in higher elevation terrain. Even a small slide can have serious consequences in big, steep terrain or if you’re above cliffs.
A short video by Greg Gagne explaining layering on an upper elevation northeasterly facing slope in White Pine where there was collapsing on Thursday.