Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1.5–2.5
It remains possible to trigger a large persistent slab avalanche that fails on weak layers buried 2-4 feet deep. These weak layers include crust facet interfaces and facets near the ground. You may not see any red flags before triggering an avalanche on these layers.
The crust facet layer is the most widespread and concerning. This layer is buried 2-3 feet deep and produces full propagation in snowpit tests, according to several recent observations. It can be a tricky persistent weak layer to manage and highly elevation dependent. This problem could be more sensitive today in areas where rain fell last night on a poor snowpack structure. If you hear whumfing or feel collapses, these are indicators that you are in an elevation band with avalanche potential. You can also dig in the snow and look for poor snowpack structure with a slab above a crust facet layer. Manage the problem with slope angle and stick to slopes less than 30 degrees. Persistent slabs could also be triggered remotely, from low angle slopes above, below, or to the side of steeper slopes.
Triggering a large and destructive persistent slab avalanche on weak snow near the ground is still possible on high-elevation northerly slopes. These are locations where early-season weak layers were buried, and were not saturated by rain earlier in December. This setup only exists in isolated locations, but the consequences will be high if you trigger one of these avalanches. Avoid slopes over 30 degrees if you find weak sugary snow with a slab above.