Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 2
A persistent weak layer of loose, sugary faceted snow exists on W-N-E aspects beneath a slab that is 2' -3' thick. This problem is most pronounced on slopes facing NW-N-NE-E near treeline and below. Above treeline the weak layer distribution is much more variable and it is hard to track, but where it does exist, wind drifted snow has has helped to overload it. In my travels yesterday, I continued to experience localized collapsing near tree line on shady slopes and stability tests continued to produce failures in snow pits. As time goes on and things begin to stabilize, outward signs of instability will lessen and we'll be more tempted to venture into steeper terrain. But with the knowledge of what's underneath, it will be hard for me to justify going on to steep, northerly facing slopes for some time.
This image illustrates the snowpack history from when it quit snowing on December 31, through now. To see how the snow nerds record this information, scroll down to additional information.