Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
An overall poor snowpack structure exists on many NW through SE 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 beneath and in some cases near the ground. Slopes that have been susceptible to previous wind events have several layers of facets sandwiched between slabs. Previous hard slabs that are now buried by the new snow from earlier in the week will feel good underfoot and may create a false sense of security. Finding the "sweet spot" such as thinner portions along the margins of the slab or around rock outcroppings can provide a better avenue for effecting buried weak layers and producing an avalanche.
Most slopes below treeline lack slab at this time, but open wind prone slopes at these elevations may have enough of a slab to be able to propagate an avalanche that could sweep you into trees or push you into a terrain trap.
Persistent weak layers in the middle of the pack and depth hoar near the ground in shallow snowpacks remain a concern, especially on slopes where you find a stiff cohesive slab.