Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
The snowpack structure in the Elkhorns remains poor. The last week has brought about 1.5" of Snow Water Equivelent. This has not been enough weight to tip the balance on the weak snowpack structure with natural avalanche activity, but the snowpack is primed and waiting for a trigger. WAC Pro observer Karen Morse has a great observation from yesterday that can be found here. She found a couple thin crusts within the upper foot of the snowpack. Two main layers of concern were identified. One was a foot from the surface, and the other was anywhere from 3-4 feet from the surface. Another great ob from last week in the Hoffer Butte area can be found here.
As time progresses, this problem will have a lower likelihood, but the consequences will remain real. We are starting to see less consistency in our snowpack tests, with some tests not showing propagation. Remember that the poor snowpack structure always trumps a "false negative" snowpack test. Snowpack tests are not decision-making tools, and offer a single data point in a sea of spatial variability. It's becoming less evident if you just look at the snow surface, as obvious signs of instability may not be present. The cracking and whumphing (collapsing) that we observed last week has decreased, and the slab may be able to hold the weight of a rider until the slab thickness decreases somewhere in the terrain.
Remember what we need for a slab avalanche? Slab + Weak Layer + Bed Surface. We've got it! When we put that in terrain steep enough to slide and introduce a trigger, we get a slab avalanche.
If you want to avoid avalanches, you should stay off of slopes greater than 30 degrees, stay well clear of avalanche runout zones, and not ride above terrain traps. Don't trust these facets until they are swimming in the river!
(1/25/2024) Photo: Karen Morse
SE 7700'