Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3.5
There are two persistent weak layers in the mid and lower snowpack. The first is a layer of surface hoar and facets from early december. This layer is most concerning at treeline and continues to produce sudden results in snowpack tests. The second is a layer of facets and a crust from mid November. This layer has not shown reactivity recently.
Be aware that storm slab avalanches have the possibility to step down to these layers resulting in larger and more destructive avalanches.