Persistent Slabs
N
NE
E
SE
S
SW
W
NW
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 3
A layer of surface hoar that was buried on January 17th should be 2 to 3 feet down from the surface. We just added a heavy new load to this layer. You're most likely to find it in wind-sheltered, shaded, and open terrain, possibly up to ridges, and east of the Cascade Crest. On the 23rd, observers continued to report signs of instability, with an extremely loud WHUMPH, that in turn triggered another WHUMPH on a Northwest aspect at 4800ft near Grace Lakes. Observations show this layer is present at Grace Lakes, Yodelin, Lichtenberg Mountain, Smithbrook, and Jove Peak areas. At lower elevations, the snow surface has become wet, and water has made its way through. The snowpack will take time to refreeze, but probably won’t do so by tomorrow. As such, it’ll be best to treat the terrain like this layer could still fail. Small and large snowpack test can help you identify this weak layer and gather information. Lack of evidence in one profile or snowpack test shouldn't be a reason to travel in more consequential terrain.
The size of the potential avalanches has just increased with the new coat of snow. As such, any avalanche on this layer would be very large and surprising.