Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
On slopes facing the north half of the compass, in some areas, it is possible to trigger slab avalanches failing on a sugary, buried persistent weak layer. These days there are few telltale signs of instability or apparent red flags, like cracking or collapsing. Today's warming temperatures could cause increasing instability on slopes plagued by this buried persistent weak layer. The warming will soften existing slabs and crust layers, and increase creep and glide rates, which could cause natural avalanches to become more possible and triggered avalanches more likely.
- In some areas, avalanches still might be triggered remotely or from a distance.