Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
Recent avalanches: A large avalanche cycle occurred with the last major storm on January 14 to 16, with very large avalanches occurring on many of the slopes in the Summit Lake area.
There are numerous avalanche problems today due to active weather and a well-documented persistent weak layer buried deeper in the snowpack. If you're still keen on recreating in the backcountry, you'll likely be spending the majority of your time in the 1,500 to 2,500' elevation band in the Summit Lake zone today. This is where you'll find the best visibility and surface conditions. Unfortunately, this is also where we're finding the persistent weak layer (crust/facet combo) still very much intact and producing unstable results in our snowpits. Currently buried ~2-3' deep, this layer is becoming more difficult for a skier or snowmachiner to trigger. It is less likely to give us the feedback we yearn for, such as shooting cracks or big whumpfs, before avalanching. The slab is deep enough now that if a skier or rider were to initiate an avalanche on this buried weak layer, it would be catastrophic. Trigger points, such as small trees or rocks breaking the snow surface, are the areas most likely to trigger a large and dangerous avalanche. If travelling in the mid-elevation band, cautious route-finding and conservative decision-making will be essential.
(1/24/2026)
It's becoming less likely that we'll get the telltale signs of an unstable snowpack the deeper the persistent weak layer gets buried. A lack of red flags doesn't mean our snowpack is any safer given the current setup. Photo: East-facing slope around 2200' on Fresno.
Photo: Andy Moderow