Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Unlikely
- Taille
- 1–2
Some starting zones on northerly and northeasterly aspects still have a weak layer near the base of the snowpack. Recent observations indicate that this weak layer, found near ground level, is diminishing. However, the distribution of this problem may vary significantly, even in adjacent locations. While triggering a slide of this type will be unlikely, the consequences will be severe. The only way to determine the presence of this problem is to examine the snowpack.
The last known avalanches resulting from a persistent weak layer occurred during the MLK Storm Cycle in mid-January. They were natural avalanches of size ~D2.