Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2.5–4
Deep Persistent slab avalanches failing within older layers of snow from late February have become a low likelihood/high consequence scenario. Human triggering of these layers is unlikely, however, potential deep slab triggers may include objective hazards such as loose wet avalanches, rockfall, or cornice fall. Solar warming may make these types of triggers a possibility today. If triggered, expect deep slabs to propagate widely, connect multiple start zones and terrain features, and run long distances to valley floors. Deep slab release is often difficult to predict, assess and manage. You can decrease your exposure to the problem by limiting time spent in complex terrain and in the tracks and runouts of large avalanche paths. Areas of heightened concern include large low-elevation terrain traps like deep canyons between mountainsides and creek beds at the entrance to alpine cirques.
(3/13/2023) Photo: Jeff Montgomery