Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–1.5
Since 12/9, several northwest-to-southwest wind events formed slabs around a foot thick or more in heavily wind-loaded terrain features. These wind-drifted slabs are most commonly found at higher elevations below leeward ridgelines and rollovers on east to northeast-facing terrain. They can also be found around the northern half of the compass in a few concave terrain features that collect drifting snow, such as gullies. These slabs are often hard and difficult to trigger, but some formed over weak, faceted snow that is slow to heal, making for variable feedback. This week, a few inches of snowfall have obscured the evidence of previous wind-loading and made it more difficult for you to identify the problem. Use caution around leeward terrain features, particularly if you feel stiff snow a few inches below the surface, as this is likely an old, hard slab.
In very isolated areas, an avalanche could release a couple feet deep on weak layers near the ground. These areas would have retained the full-season snowpack without previous slides during the widespread avalanche cycle that occurred in late November.
This small hard slab was skier-triggered near Mt. Tilton on 12/20. Note how the slab is in a concave, previously wind-loaded feature.