Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2.5–3.5
Weak snow buried near the base of the snowpack continues to present 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 that we have observed over the past weeks, in conjunction with our field observations, indicate that this layer is at its weakest on the northern half of the compass.
In the Banner Summit area this layer is now buried 4-5+' below the current snow surface underneath a very dense slab of snow. As this slab grows, it is making it harder and harder for us to impact the weak layer. 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, wind slabs failing in the upper snowpack, and finding a thinner spot in the snow cover are "good" ways to trigger these slides as well. 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'.