Storm Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 2–2.5
More wet, heavy snow is building another storm snow layer on the surface. These slabs are forming above a harder interface where rain saturated the snowpack then refroze, or onto prior snowfall at elevations above the rain line. To keep things simple, this is adding more depth of recent snow and weight to a snowpack that has shown it's true colors in the last few days. The significant hardness difference between the storm snow of the last few days to what accumulated earlier in the month is a major factor of the elevated sensitivity. Dense slabs of snow have a higher potential to break wider than you expect, even in wind-sheltered areas. If you're lucky to only observe signs of unstable snow like cracking or collapsing without triggering an avalanche, that's good fortune. Simply avoid exposing yourself or your group to steeper slopes until the new snow has a chance to catch a breath.
(1/1/2025)
A shallow, soft slab avalanche failing in the recent storm snow. Bitterroot Mountains. January 1, 2025.
Photo: Izzy Davis