Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3
Slabs over buried weak layers 1.5 to 3 feet thick are typically stubborn to trigger. Obvious signs of instability are rare, and avalanches are most likely triggered from where slabs are thinner. The north half of the compass has the most fragile weak layers buried in the middle and bottom of the snowpack and is most likely to produce remote-triggered, widely propagating, or destructive avalanches from steep or adjacent flat terrain (see several videos illustrating this). At the lowest elevations, slabs may take on a moist or wetter flavor today. Some higher-elevation southerly terrain also harbors problematic structures. The most reliable strategy for managing this problem is to choose conservative slope angles or travel on mid- to low-elevation southerly aspects. Avoid traveling in or near steep terrain with variable snow depths or trigger points.
A pair of large persistent slabs below Scarp Ridge, which likely ran during increased winds on Tuesday, 2/24.
Photo: Irwin Guides