Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–3
What and where is it: You could 1.5-4 foot thick slabs, especially where wind formed drifts or stiffened the snow surface. Triggering an avalanche is less likely—but not out of the question—on steep slopes that are completely sheltered from the wind. The slabs rest above a variety of weak layers (facets, surface hoar, crusts, and combinations). The widespread nature of the weak layers means avalanches are possible on many aspects.
How can you recognize it: Snowpack cracking (photo), and collapsing or whumpfing, are clear signs of unstable conditions. Watch for snow pillows, dunes, and ripples (photo), and feel for stiff snow under your feet or sled. These are signs the wind has been at work transporting snow. Assume the weak layers exist on most slopes.
How can you manage it: You can avoid steep, wind-loaded slopes to significantly reduce your chances of triggering an avalanche. Persistent Slabs can release in surprising ways, break wider than expected, and release above or hundreds of feet away from where they are triggered. Remotely triggering an avalanche from flat terrain near steep slopes is a real possibility. Keep a close eye on your partner and the terrain that's above you.
(12/29/2024) This persistent slab avalanche was remotely triggered from gentle terrain above the crown. NW slope near 8600' in the Prairie Ck drainage of the Smoky Mtns.
Photo: Jon Preuss