Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
As we get further out from the weekend's storm, obvious signs of instability are decreasing. However, lower density storm snow over the 1/10 crust is still yielding mixed results in snowpack tests, and we just don't fully trust this bond yet. It will likely take a steep slope with a thicker slab to trigger an avalanche, and unsupported or convex features are all the more suspect. The tops of chutes, aprons at the base of cliffs, and slopes below steep ridge lines are all likely locations to find this problem. You can use hand pits and small test slopes to gauge for reactivity, but you need to be sure that the test slope is representative of the start zone on the slope you are considering. Subtle differences in slope angle, aspect, and wind-deposition patterns can make a huge difference in slab presence and reactivity. The simpler and safer move is to give wind-loaded slopes over 35 degrees another day to settle out. Choose supported, planar slopes where you don't see signs of wind-drifting.
(1/13/2025)
A look up at the crown of a human-triggered wind slab avalanche from 1/11 on a northeast-facing slope at Alpental. This avalanche broke on a 40-degree slope at the base of cliffs–an ideal location for a wind slab avalanche on Tuesday.
Photo: Josh Lipkowitz