Deep Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2.5–3.5
Weak snow buried near the base of the snowpack poses a significant hazard here. This snow fell during the month of October and was preserved on many middle elevation slopes that face away from the sun (E-NE-N-NW), and on most slopes at upper elevations. The pattern of natural avalanche activity combined with our field observations indicate that this layer is at its weakest on the northern half of the compass. I made a video yesterday to try to help explain where you will find this snow and why that is important, you can watch it here. I think it is worth your time.
In the Banner Summit area this layer is now buried 4-5+' below the snow surface underneath a very dense slab of snow. As this slab grows and stiffens it becomes harder and harder for us to impact the weak layer beneath. However, any avalanche that fails on this weak snow will be very large and destructive. Dropping the track of your sled into this weak layer is a "great" way to impact it. Large cornices collapsing and wind slabs failing in the upper snowpack can also be good triggers for deeper weak layers. Finding a place where the overlying slab is thinner, such as in steep, rocky alpine terrain will greatly increase your chances of triggering one of these monsters. Avalanches may be triggered remotely—from flatter terrain below, above, and to the sides of steep slopes.
(12/24/2021) Very large natural avalanche on "Marshall Slide" in the Sawtooths, on the shoulder of Williams Peak, above the Marshall drainage. This avalanche appears to have failed in the October facets deep in the snowpack. NE-aspect at 9,000'.