Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
What is it? 1-3 foot thick slabs overlie persistent weak layers (sugary facets, surface hoar, and/or crusts) on many slopes. Recently wind-loaded slopes are the most dangerous. The photo to the right/below is a great example of a medium-sized avalanche that you might trigger in very steep terrain that is somewhat sheltered from the wind.
Where is it? Most slopes harbor at least one of several weak layers in the upper part of the snowpack, but you're most likely to trigger avalanches on slopes where the wind has formed drifts or slabs or stiffened the snow at the surface (example photo). Wind-exposed bowls and slopes near ridgelines, prominent gullies, and chutes are most likely to produce large avalanches. Unfortunately, you cannot assume wind-sheltered slopes are safe.
How can you recognize it? Assume this problem exists until proven otherwise. You may or may not 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.
How can you manage it? Unfortunately, avoiding slopes steep enough to slide is the only surefire way to manage this problem. Persistent slab avalanches are tricky. These avalanches may break wider than expected or higher on the slope above you. You may be able to trigger avalanches remotely—from gentler terrain below, above, and to the sides of steep slopes.
ADDITIONAL DISCUSSION: While triggering slides on faceted snow deep in the snowpack is unlikely, it can't be ruled out in steep, rocky, wind-affected alpine terrain. Slopes like these have variable snow depths, and thinner snowpack areas allow our weight to more easily impact deeply buried weak layers.
(1/10/2023)
Snowmobilers remotely triggered this thin but wide avalanche from flat terrain a ways below the slide. Smiley Ck drainage, NW aspect near 9000'.