Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
Very weak faceted snow exists near the ground on almost all northerly-facing slopes at upper and mid-elevations. While definitive signs of instability like collapsing are waning, the poor snowpack structure hasn't gone anywhere. It is still our top concern and not to be trifled with. Eventually it will be buried deeply enough to not pose a problem but we are not there just yet. We need to give these slopes more time to heal. The list of popular slopes that have yet to avalanche includes the Rodeo and Fairgrounds Bowls on the east side of Logan Peak, 3-Terraces, and the north face of Providence Peak, the east face of Mt Magog, Double Top, as well as Wilderness Peak, St. Charles, Slide Canyon, and many more.....
- Recent avalanches, shooting cracks, and collapsing (whumpfs) are signs of unstable snow, but these obvious signs of instability will not always be present when a large avalanche occurs.
- Avalanches could be triggered remotely (from a distance) or worse, from below steep slopes in the flats.
A large natural avalanche on Cornice Ridge that likely occurred in the overnight hours of 12/28-12/29. It got filled back in with snow but likely failed on the PWL.