Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
What is it? A 3-4 foot thick slab overlies persistent weak layers (sugary facets, surface hoar, or crusts) on most slopes The slab is harder and denser near Banner Summit than in our other zones, making it a little less sensitive to triggering by skiers and snowmobilers. Slopes sheltered from the wind are suspect, and recently wind-loaded slopes are more dangerous.
Where is it? The recent storm added to the slab everywhere, and the weak layers are widespread. Conditions are unusually dangerous in lower elevation terrain.
How can you recognize it? This persistent slab problem is about as widespread as it gets; assume it exists on all slopes until proven otherwise. You're likely to experience snowpack collapsing and/or cracking while traveling. These red flags are obvious signs of instability. Wind-loaded areas feel stiffer under your skis or sled and keep you from easily sinking into the snowpack; these areas are especially dangerous.
How can you manage it? Avoiding slopes steep enough to slide is the only surefire way to manage this problem.Persistent slab avalanches are tricky. If you're playing near steep slopes, you could trigger slides remotely (from gentler terrain above, below, and to the sides of steep slopes—explanatory video here). These avalanches may break wider than expected or higher on the slope above you.
(12/12/2022) In the Banner Summit zone, the weak November snow is buried beneath a 3' thick dense slab.