Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
In this zone there are two separate persistent slab problems to think about:
- Recent natural avalanche activity indicates that a recently buried interface in the upper portion of the snowpack continues to be capable of producing avalanches. I observed one such slide yesterday in the Frenchman’s drainage near the headwaters of the Salmon River (photo). The slide appeared to have failed on Sunday.
- Weak snow exists near the base of the snowpack. This snow was the culprit layer in a widespread avalanche cycle that took place during last week’s storms. Chris reported that this was one of the most extensive deep slab avalanche cycles in recent memory. Avalanches failing thousands of feet wide were observed in many cirques.
You are more likely to encounter the first of these problems. The shallow weak layer is much closer to the surface and your chances of triggering an avalanche involving it are greater. However, if you are trying to avoid exposure to avalanche hazard entirely, you have to be mindful of the monster lurking in the basement. Avoiding this problem means avoiding the terrain that this problem exists in. You’re most likely to trigger one of these avalanches in terrain where there are shallow, rocky areas that allow you to impact the weak layer. Areas where the wind created slabs and added weight to this weak snow will also be more sensitive to human-triggering. Triggering an avalanche on a near-surface weak layer may result in a much larger, deeper avalanche as it moves downhill.
ADDITIONAL DISCUSSIONPrecipitation starts again this afternoon. Wind speed will increase a bit late in the day and overnight as the storm exits our area, shifting from SW to NW. Fresh wind slabs will be small, but may be touchy. More importantly, these slabs will add stress to the weak snow underneath. Also, one of these much smaller, fresh slabs may be able to trigger a larger, deeper slab as it travels downslope.