Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–3
Almost every storm cycle, we have buried surface hoar. The mountains received over 2 feet of new snow over the last week. We now have a soft slab about 2-2.5 feet deep that formed over weaker snow and crusts below, which was the cause of the avalanche cycle last week. 3 skier triggered avalanches have occurred in the last 3 days at the new/old snow interface up Lick Cr Canyon---one of these we remote triggered from the ridge when we felt and heard a large whoomph.
Both of the other reported skier triggered avalanches, people described easy and rapid propagation over a large area on a slick crust. Triggering this slab is getting harder in most places as it is gaining strength, but as we found yesterday, it is vey well preserved and very sensitive or weak in protected areas.
Check your slope angles, and think about where might the weak layers have been able to survive the Sun and wind...Avoiding steep terrain and only putting one person at a time on a slope is still your best bet. Adding the weight of new snow to these weak layers will be a test of the strength of them.