Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
The cold dry spell in November created a very weak snow surface composed of near surface facets and surface hoar on almost all aspects and elevations throughout the Wasatch. This layer was subsequently buried on the 27th of November and is now reacting to the new load on top of it. The weak layer is present and has been the guilty party in a number of recent avalanches. We are still trying to determine where the weak layer is present and will give suspect slopes a wide berth until we can show that the weak layer doesn't exist.
Recent high winds from the south added an additional very hard wind slab on top of this weak layer which has led to avalanches being triggered naturally and remotely to skiers and snowmobilers up to 6' deep and 300' wide. Today's new snow plus any possible wind drifting will make more avalanches likely today. These are unsurvivable avalanches. Any steep slope is suspect until proven otherwise and the best travel advice would be to avoid slopes over 30 degrees. Based on recent activity this travel advice includes any slope with overhanging terrain where you might trigger these facets from a distance.