Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
Wind loading has been the primary mechanism creating stress on the 1/26 persistent weak layer. Currently, there is little to no snow available for transport, and therefore, no added stress is being applied to the weak layer. We expect the chances of triggering an avalanche on this layer to be decreasing, but there is some uncertainty regarding sensitivity in heavily wind-loaded areas. Specific leeward terrain features, including steep gullies and large cross-loaded slopes, will be the areas where this problem exists. Winslabs up to 3 feet are expected have decreasing reactivity, but could be sensitive where the slab is thinner. This problem has been slow to heal, as evidenced by several separate avalanche cycles over the last month. Due to the high consequences of triggering this problem, careful terrain management is advised. Users can reduce their risk by avoiding large connected alpine faces and slopes that have been previously loaded by wind. Given the brutal conditions out there, it should be an easy decision to stay off hazardous terrain today.
Expect to find significant variability with this problem. Windward areas and exposed slopes will be stripped of the overlying slab that is creating this problem, while leeward slopes will have deep wind-deposited hardslabs.
(2/21/2026)
HS-N-R2-D3-O
Natural persistent slab avalanche on Averys/SW that failed at a PWL on 2/20 and ran full path ~3800'.
Photo: Gareth Brown