Storm Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
You asked, and Ullr provided. In the 48 hours since snow began on Sunday, Hatcher Pass has received over two feet of snow, doubling our snowpack.
As you climb in elevation into more wind-exposed terrain, it won't take much southerly winds to have moved this low-density snow around, creating a stiffer, more sensitive slab. These are the areas where you may trigger wider avalanches that could bury or injure a skier or rider—especially on slopes with gullies, concavities, or cliffs. Watch for cracking or collapsing within the new snow; this is evidence that you have found a consolidated slab of new snow capable of making avalanches.
At low elevations or in sheltered terrain, triggering a slab avalanche is less likely, but in steep terrain, you could trigger loose snow avalanches or sloughs that could knock you down and carry you where you don't want to go. These slides may gouge into the old weak snow near the ground—creating larger, more consequential avalanches.
A cooling trend at the end of the storm should contribute to slabs loosening and becoming less reactive throughout the day, but remember this mantra: You are most likely to trigger new snow avalanches during the storm and up to 48 hours after it finishes. Hand pits and small test slopes are good indicators that a slab is still cohesive and could still avalanche on steeper slopes.
We experienced widespread cracking within new storm snow throughout the forecast area. In places where new snow overlays weak sugary snow, it was easy to get it to entrain on test slopes.
Photo: Hatcher Pass Avalanche Center