Storm Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
The main avalanche issue is a layer of dense snow resting on a layer of very light and fragile snowflakes. This light snow fell at the start of Sunday's storm and was the weak layer in many of yesterday's avalanches. On many slopes this layer rest on top of an ice crust or other firm layers allowing avalanches to run far.
Normally, weak layers of soft new snow can stabilize quickly. What is unique about layering in the upper 2 feet of the snowpack is dramatic hardness differences. These differences should keep this avalanche issue alive today. You can easily feel these changes in hardness if you dig with your shovel or poke into the snow with a ski pole.
Another issue that may keep the new snow unstable a little longer than normal is the possibility of some weak faceted snow on top of a crust that formed on Feb 7th. I don't think this is a widespread issue, but we have a lot of uncertainty about it and will be looking for it this week.
Photo below of the new snow layering and where fractures are most likely to occur and produce avalanches.
Danger trend: decreasing