Storm Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
A weak upper snowpack exists throughout the zone. Crusts, buried weak grains, and low-density snow will be capped by rapid wind-loading or snow falling on a warming trend. As the snow stacks up and the wind redistributes what's already on the ground, the likelihood of triggering an avalanche will increase. You may even witness natural slides.
Look for heavy snow over weaker snow, shooting cracks, whumpfing collapses, or new avalanche activity as an indication that avalanche potential is on the rise. With our unconventional PNW snowpack, any triggered avalanche could step down to deeper layers, breaking widely or in surprising ways.
Don't leave it to chance. If you notice red flag signs of avalanche activity, default to slopes below 35 degrees.
(2/19/2026)
A large human-triggered avalanche that fully buried a snowmobiler at Mount St. Helens on 2/19. The failure layer is unknown. [HS-AM-R2-D2-U, NE, 6000 ft.]
Photo: Northwest Avalanche Center