Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1.5–3
The chance of triggering large avalanches is greatest on recently wind-loaded slopes over about 35 degrees. We have two persistent slab problems to consider:
- "Fresh" Slabs: You could trigger 1-2 foot thick slides on middle and upper elevation slopes. The new snow that fell over the past several days has formed a soft slab above small facets or crust + facet combinations. These slabs are thicker and more dense in terrain exposed to the wind. In more sheltered terrain, triggering slides is less likely but still possible on slopes approaching 40 degrees. Watch for obvious signs of instability like snowpack cracking or collapsing.
- Thicker, Older Slabs: While unlikely, the possibility of triggering a massive 2-5 foot thick avalanche remains on the table. These hard slabs also rest on weak facets and crust + facet combinations. This problem has been "quiet" this week, meaning we haven't observed recent avalanches or snowpack collapsing. That said, the poor structure (slab over weak snow) and track record (hundreds of natural avalanches around St Patrick's Day) are hard to ignore. Smaller avalanches running downslope could step down to this weak layer, triggering an unsurvivable avalanche. You probably won't see any obvious signs of instability associated with the thicker slabs, and there's an outside chance you could trigger these beasts remotely—from gentler terrain above, below, and to the sides of steep slopes.
The combination of widespread weak layers, a developing persistent slab problem in the upper 2 feet of the snowpack, and the uncertainty associated with deeper weak layers adds up to variable, spooky conditions in avalanche starting zones. Triggering avalanches is much less likely on slopes sheltered from the wind that are closer to 30 degrees in steepness.