Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Numerous avalanches have been reported since our last storm indicating that buried weak layers are still reactive and adjusting to the snowpack. Slab depths above these weak layers are 1-2 deep with locally higher amounts in upper elevations on previously wind loaded terrain. You will most likely find this problem on slopes facing NE-N-NW above about 8,500’. On these aspects and elevations, preserved snow from early fall has created a weak snowpack structure that is sensitive to remote triggering. Analyze the terrain you travel in carefully to avoid being caught off guard by the unpredictable nature of this type of problem. Look for any cracking and collapsing as these are obvious signs of instability.
This observation above Triple Direct is a good example of an avalanche being remotely triggered.
(12/5/2023)
This photo accurately depicts the current persisent slab problem and remote triggering from gentle terrian above, below, or to the side of steep slopes.
Photo: Travis Baldwin