Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
We now have two buried weak layers in our immature snowpack. One is a layer of facets located 1"-8" off the ground and the other is a buried surface weakness that formed during the early December high pressure and is just under the newest snow. The one near the ground is easy to see in snowpits and is the classic weak snow with strong snow over the top. The harder to find surface weakness is now buried 6"-12" under the most recent new snow and wind. This weak snow will be spotty as it may have been destroyed by high winds and warm temperatures before it was buried by the most recent storm snow. Many of our backcountry observations have included reports of collapsing, cracking, and whumpfing. These are all signs that the snowpack is adjusting and if you see/hear these signs, or see recent avalanche activity then back off and find a lower angle slope to travel on.
Photo (T) with the red arrow pointing to the thin gray line of buried surface hoar (surface weakness) from upper Little Cottonwood Canyon.