Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
Decision making for me is really simple. I would stay off any slope that held old snow prior to last week. This old snow is nearly a foot thick and has formed a persistent weak layer of facets at the ground. Snowfall last week overloaded this weak layer and produced a widespread avalanche cycle. A soft slab 2-3 feet thick rest on this weak layer now. The diagram or "rose" shows where this persistent weak layer exists by aspect and elevation - slopes above 9500 feet facing W, NW, N, NE, E, and SE north, & slopes between 8000 and 9500 feet facing NW, N, NE, and E.
Triggering an avalanche on this weak layer remains likely. The resulting avalanche would be 2-3 feet deep (or more on wind loaded slopes) and would break hundreds of feet wide. Unfortunately, this avalanche problem is here to stay. Through time it may become more stubborn to trigger but the threat will remain. Sunday/Monday's southerly winds drifted snow and provided additional loading to many of these slopes. More load = more stress = avalanches.
The only way to avoid this problem is to ride slopes less than 30 degrees in steepness which aren't steep enough to slide. Also, avoid being under any steep slope because you could still trigger these avalanches from below and have one crash down on you. View a simulation of how this happens HERE.
Photo (B. Torrey) below shows this simple layering of this avalanche problem - a soft slab of snow resting on this persistent weak layer.