Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 2–3
What is it? A very dense, 2-4+ foot thick slab stands over buried weak layers of facets or crust + facet combinations. While these avalanches are getting harder to trigger, releasing these destructive beasts is not impossible. Watch the video to the right/above to understand this problem better.
Where is it? Most slopes harbor these layers. You'll find crust + facet combinations on sunny slopes and small facets on shaded slopes. We are still tallying up the historical amount of slides produced by these weak layers (map, list).
How can you recognize it? The first sign of instability may be the large, destructive avalanche you trigger. Tracks on a slope don't indicate it is good to go. These slides may break much wider and further above you on the slope than expected. Unless you dig down to confirm the weak layer exists, you might assume the snowpack feels good under your feet or sled. And if you take the time to dig down, don't trust the results of your stability tests. They serve little help when dealing with such a dense slab overlying this weak layer.
How can you manage it? The only way to eliminate your risk of encountering one of these devastating slides is to avoid avalanche terrain and terrain exposed to hazard from above. I know that's not satisfying to hear. You can reduce your risk by avoiding slopes steeper than about 35 degrees—especially large avalanche paths and those with ugly consequences if caught in a slide. Remember that even small slopes can have high consequences when dealing with very dense slabs. These slides can be triggered remotely—from gentler terrain above, below, and to the sides of steep slopes.
ADDITIONAL DISCUSSION: You are more likely to find older wind slabs in the Dollarhide area, where more snow has fallen over the last week. These small avalanches will be isolated to ridgelines in upper elevations and further down the slope on the sides of gullies and ribs. Steer away from avalanche terrain when your skis or sled come across denser snow. These slides can be effective triggers for releasing a larger avalanche deeper in the snowpack.