Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A persistent weak layer of October and November facets makes up the base of the snowpack on north-facing slopes at mid and upper elevations. This is primarily on west, through the north, through the east-facing aspects - but may extend all the way to southeast-facing aspects in the upper elevations as well.In these areas, it is still possible to trigger an avalanche up to about 1-2 feet deep and over 100 feet wide.
This setup was obvious over the weekend, with widespread avalanche activity and plenty of red flags. As we move farther from the loading event, those signs may be less obvious, but the structure has not changed. Sensitivity and overall likelihood are slowly dropping, but the consequences remain high.
This problem extends across both mid and upper elevations, and both deserve caution. Upper elevation slopes remain the most suspect because they received the most snow and have the most connected weak layer.