Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2
Southwest winds have formed dense surface slabs on layers of surface hoar that were buried on January 16, 11 and 2. These buried persistent weak layers are potential failure surfaces for slab avalanches. At the mid and upper elevations these surface slabs will become increasingly sensitive to human triggers and are likely to fail on the January 16 or 11 layers with depths up to two feet. Some potential may exist for these slabs to step down to the January 2 layer with depths to three feet. Shallow wet loose slides and pockets of dense or wet surface slab up to a foot deep are possible in steep terrain at the lower elevations.