Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2–3
Recent avalanches: The last known avalanche activity in the Seward and Lost Lake zone was during and immediately after the atmospheric river event, which occurred just over a week ago, between January 16th and 19th.
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 1,000 to 2,500' elevation band 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 as recently as yesterday. Currently buried ~2-5' deep, this layer is becoming more difficult for a skier or snowmachiner to trigger. It is unlikely to give us any 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.
In lower elevations, below about 1,000', the snowpack is thin, and unfortunately, we are seeing more rain today. There is, however, enough snow in the mid and upper elevations that it's possible debris could reach below 1,000' in funnelled terrain.