Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1.5–3
Many slopes have weak snow at the bottom of the snowpack, and new slabs have formed over persistent weak layers in the upper snowpack which are reactive to the weight of a human. A triggered avalanche in the upper snowpack could step down to deeper weak layers near the ground, becoming much larger than expected, and producing a destructive avalanche. This avalanche problem can propagate widely through the terrain, or be remotely triggered from low-angle slopes connected to steeper slopes.
Avalanches could step down into deeper weak layers such as this human-triggered avalanche on 12/27.