Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Last week's heavy snow created a more cohesive slab on widespread preexisting layers of very weak faceted snow. In many areas the overload of heavy new snow was just enough to activate these layers and cause dangerous slab avalanches. More snow fell and drifting occurred Sunday, which continued to load slopes with poor snow structure. On slopes facing the north half of the compass, people are likely to trigger soft slab avalanches failing on a buried persistent weak layer. Persistent weak layers consisting of faceted snow sandwiched between crusts exist in some more sunny terrain, and some may be becoming active now as they are overloaded by drifted snow. Observers in the Logan Zone have reported signs of instability in the backcountry, across the zone, including audible collapsing and cracking.
- Avalanches could be triggered remotely or from a distance.
- Shooting cracks and audible collapsing are red flags indicating unstable snow.
An observer triggered these deep shooting cracks yesterday at around 9000' on a northeast facing slope in the Central Bear River Range.