Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
As described above, a layer of very small facets next to an ice crust has been producing slab avalanches. If the issue was solely the new snow, then this problem would have stabilized by now. Unfortunately this layer will continue to be a concern, but it shouldn't last nearly as long as other persistent weak layers. A process currently occurring again on the snow surface (described in this video) likely formed this layer early last week during cold temperatures and brief moment of clear weather.
Here's the good news - This layer mostly exists on slopes that should have an ice crust on the surface this morning, and those are ones you will likely avoid anyway. Northerly facing slopes seem to lack this layer and will have better snow.
Photo of this layer from an avalanche on a southwest facing slope in Little Cottonwood Canyon (photo - Little).