Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
An overall poor snowpack structure exists on many Northwest through East slopes near and above treeline. It's on these slopes that you're most likely to find stiff cohesive slabs over very weak faceted snow. A strong wind event just before Christmas developed stiff hard slabs that now have settled storm snow from Dec 29 resting on top. Prolonged periods of high pressure earlier in this season have formed uniform weak layers of facets and depth hoar throughout our snowpack.
Triggering an avalanche on one of these weak layers has become increasingly stubborn as we become further removed from our last loading event. You are most likely to trigger an avalanche on these slopes over areas where the slab is thinnest such as around rock outcroppings and on the margins of the slab. You can mitigate this hazard by avoiding slopes greater than 35 degrees.
We continue to find a similar snowpack structure on NW through E slopes near and above treeline. The weak layer of concern continues to be small grained facets beneath the hard slab.