Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Hard slabs 3-5 feet thick overlay weak snow that formed earlier in the season. Shallow, rocky, and unsupported terrain on the north half of the compass is where this problem has been most active. It is currently unlikely that a human would trigger one of these slabs. Larger triggers, like cornice fall or surface snow avalanches (i.e., wind slabs or wet avalanches), can impact weak layers buried deeply in the snowpack and initiate a much larger avalanche. Furthermore, an extreme loading event or a prolonged period above freezing has the potential to impact these layers.
(3/5/2024)
A very large persistent slab avalanche failed during the early March storm cycle. This terrain characterizes where this problem is most active: very steep, unsupported slopes near cliffs.
Photo: Dan Hayes