Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
There is a reason that the avalanche danger is LOW in this zone - it just refuses to snow down here. The "favored" portions of this zone have tallied 2" of snowfall in the past 2 weeks. The last significant reported avalanche took place 12 days ago when ski patrollers at Bald Mountain intentionally triggered an avalanche during avalanche mitigation work. The slide failed on a heavily wind-loaded slope with weak, sugary, faceted snow in the lower part of the snowpack. When you're out in the mountains today, this is precisely the type of scenario that you should be looking for: strong, dense slabs of wind-drifted snow sitting on top of weak snow near the ground.
If you're on skis or a board, try to push your pole to the ground and see if you can feel a change in resistance as you do. If you are struggling to push your pole into the snow and then all of the sudden the last bit to the ground has almost no resistance you've likely found an area where a hard slab is sitting on weak snow underneath. If you're out riding and are getting bucked around on hard snow, struggling to keep your sled cold you are likely on a hard slab of wind drifted snow. Then, you look over and that one buddy of yours who always gets his sled stuck (we've all got one) managed to punch through the hard slab and the tail end of his sled is sitting on the ground. The sugary snow near the ground that his track is spinning against is the weak, faceted snow that we are talking about here.