Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 3
It still remains possible to trigger a deadly 2-5 ft deep slab on a persistent weak layer near the ground on NW, N, NE and E facing slopes. After a couple days of sunshine and no recent avalanche activity reported, the temptation to step out onto untracked high-north facing terrain is undeniable. The issue we face is that the weak snow lurking under the surface is far from gone. In this situation, time continues to be our friend. How much time is hard to say because the odds of triggering an avalanche decrease a little with each day.
There will come a time we can begin pushing it out onto upper-elevation north-facing slopes with confidence, but that time isn't quite here yet. Just because the likelihood has decreased doesn't mean the problem no longer exists. If you choose to ride slopes where this layer exists, stack the odds in your favor by choosing slopes with a clean runout zone free of trees and rocks that would cause trauma if you do trigger an avalanche.
Throughout the week winds have blown from the north, west, and southwest with gusts above 40 mph at times. Additional wind-loading on north-facing slopes that have the persistent weak layer will increase the chances of triggering a large avalanche. Look for signs of wind drifted snow and avoid those areas.
Info about this layer and where it exists
A photo from the Park City Ridgeline shows a persistent weak layer exists near the ground. While the improving stability test scores are a positive sign, the overall poor structure still remains a concern. (photo: PJM)