Very weak faceted snow exists near the ground on almost all northerly-facing slopes at upper and mid-elevations. Other persistent weak layers have also been observed higher in the snowpack. Large and dangerous avalanches failing on a persistent weak layer are likely in drifted terrain, and they are possible even in sheltered areas. There were some impressive natural avalanches with last weekend's productive storm, but many of the most suspect slopes in the area have not yet avalanched and may be hanging in a delicate balance, just waiting for a trigger. 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.