Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–3
Several weak layers exist within our snowpack. Surface hoar, near-surface facets, density changes caused by wind and temperature fluctuations, grauple, sun and rain crusts...you name them, we have them. The take-home point is that our snowpack is complex and varied right now. Not all of these layers are found in all areas, several of them may be found in one area. ALL of them should give you reason for concern and a healthy suspicion of the snowpack. The buried surface hoar near 65cm/25in is the most dangerous. This layer is resting just above the rain crust that was buried on 1/26. This layer is incredibly reactive in some areas and not present in others. Steep slopes in wind-protected or wind-loaded, shady terrain is where you are most likely to find it. This is the layer that has been producing human triggered avalanches for almost 2 weeks. Persistent grain types have also formed this week on the snow surface and will increase the avalanche hazard as we add new storm and windblown snow over the next few days.
The most repeated message from Avalanche Centers across the Western US right now is "avoid steep slopes", with human triggered avalanches and avalanche fatalities continuing to stack up, pay attention to your slope angles and keep an eye on your partners.
Friday 2/12 Wildwood Bowl. North of Tamarack Ski Resort boundry