Storm Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
Continued snowfall will only increase the potential size of slabs throughout the zone. Slabs will be larger in wind-loaded terrain or on the volcanoes where storm totals are higher. Whether you encounter a classic storm slab due to a warming trend making the snow upside down, a poor bond with the underlying surface, or maybe a wind slab, it doesn't really matter. You will want to steer around slopes over 35 degrees and convexities where triggering a slide is more likely. You can use small test slopes or quick handpits as you travel to look for potential points of failure and help understand how the snow reacts to your weight as a traveler. With various surfaces buried by this storm, you may find that the new snow has bonded differently from slope to slope. In some locations, avalanches could fail on weak snow, breaking more easily or widely than you're used to. You may even observe natural avalanches occur during or shortly after periods of heavy precipitation or wind.
(2/15/2025)
A handful of natural slab avalanches were reported on Mount Adams on Sunday. Many of them occurred near rocky features or on convex slopes.
Photo: JB