Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 1–2.5
A rain crust from the first week of December is now buried down 30-75cm. This rain crust is widespread and can be found to mountain top throughout the regions. It has been most reactive where a thin layer of sugary facet crystals overlays it.
In sheltered treeline locations there is a buried surface hoar layer that is buried down 25-60cm. This weak layer has shown most signs of reactivity on northern aspects.
These layers have shown widespread signs of instability in recent days, including remote avalanches, accidental skier triggered avalanches, cracking and easy sudden snow test results. As these layers are more deeply buried, they may be less predictable to trigger but the resultant avalanche will be more destructive. Smaller loose snow "sluffing" or a small slab avalanche may trigger this layer in a step down event.