Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–2
Wind slabs that are variable in size and distribution are common throughout east-facing and south-facing avalanche terrain today at the middle and upper elevations. Firm slabs up to 3 feet thick have formed from an increasing northwesterly wind. Expect to find a strong-over-weak slab structure which is sitting on top of a very firm, slick crust. Especially where slabs are softer to the touch, avalanches from the weight of a person are possible. It will be important to investigate the strength of the bond between the new and old snow before committing to a slope.
Remember, snow in the starting zones and higher up in the terrain can be more reactive and form larger slabs than snow lower down in the avalanche path or in the runout. Assessing snow low down in an avalanche path is not always representative of what is up higher.