Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Weak sugary grains of facets and depth hoar still lay at the base of our snowpack. The depth and distribution of these grains varies greatly around our forecast region. In areas where the snowpack is shallower, this layer is easier to disturb. Where it is buried deeper, it is harder to initiate a failure. However, if triggered, an avalanche may involve the whole snowpack, and could have deadly consequences. Cracking, collapsing and wumpfing are all signs of this instability. Probing the snow as you travel can help you understand how deep this layer is. It is important to avoid trigger points such as rocks and trees, convexities, and steep terrain near rocky cliffs where the snowpack may be shallower. Some of these trigger points may be buried in areas with a deeper snowpack, which makes this problem even more difficult to manage. The best way to navigate this instability is to avoid traveling on and beneath slopes greather than 30º.
(1/17/2024)
Profile of a trigger point for a slope scale collapse at 9,600' on a N aspect, in the Mammoth Lakes Basin. The persistent weak layer of Faceted grains bured on 1/2/24 is near the surface above the rock slab and drops deeper where the height of snow is over a meter. The snow was weaker in this area than on the wind-loaded slope I had just crossed. My weight broke into the weak layer and caused the whole slope to collapse.
Photo: Everett Phillips