Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2.5
Weak layers near the bottom of the snowpack are persisting below hard slabs 2-4 feet deep. This problem is most prominent on shaded aspects on the northerly half of the compass (NW-N-NE aspects) that have harbored weak snow the longest. All slopes highlighted in the aspect/elevation diagram above should remain suspect as these avalanches can behave in unpredictable patterns. Obvious signs of instability such as collapsing may not be present. Despite the lack of clues, remember it is still possible to trigger large, dangerous avalanches. Identify areas that remain the most suspect on rocky, unsupported, and wind affected slopes over 35° steep. These slopes contain thin, sensitive trigger points where it is easier to impact the buried weak layer, initiate a collapse, and cause an avalanche that can travel far across or upslope.
(1/5/2025)
Looking up from the burial site at the remotely-triggered large avalanche off the west shoulder of Brooks Lake Mountain near Breccia.
Photo: Bridger-Teton Avalanche Center