Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
The Logan area mountains developed a widespread layer of weak and sugary surface snow in late January. In sunny terrain, weak layers formed under and above crusts or formed crust/facet sandwiches. Drifting and recent accumulations built thick slabs on the layers of weak faceted snow, and now many slopes are plagued by a persistent weak layer buried 1 to 3 feet deep. Today, people are likely to trigger dangerous slab avalanches failing on this persistent weak layer, possibly even in sheltered terrain.
- Avalanches could be triggered remotely (from a distance) or from below.
- Audible collapses of whumpfs and shooting cracks are sure signs of instability.