Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 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. Don't let it be you! Check out a recent observation from the Elkhorns here and here. There are well-developed, large-grained facets at the January 4th interface, and more junk in the trunk (weak sugar snow) near the ground. This weak snow is found between 2-4 feet from the snow surface in deeper snowpack areas. All of the snow since January 4th has consolidated into a dense slab and sits above weak snow with some decomposing crusts below the weak snow. Remember what we need for a slab avalanche? Slab + Weak Layer + Bed Surface. 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!