Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1.5–2.5
Slabs will grow in size and reactivity as the snow falls and loads onto lee slopes. Where slab development remains soft, these slabs will become easy to trigger, but if the slabs are hard, they could be larger, more dangerous, and widely propagating. Note the difference as you travel, using small test slopes to check for firm over weak layering. If the slabs become punchy and more supportive, you're into hard slabs, a sign that the winds have pulverized the snow grains. In most cases, slabs will form over a new/old snow interface, but the old snow frequently overlies crusts. If you engage with wind loaded aspects, choose slopes less than 35 degrees and expect that slabs could form well down below ridgelines and would be difficult to navigate around given the strength and duration of the winds.
Example: Hard slab debris. You don't want to get caught in something like this.
Photo: Joe Dellaporta