Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1.5–2.5
In the last two weeks, the majority of slab avalanche activity has occurred on a layer of facets that was buried on 3/23. The last persistent slab avalanche was human-triggered on 4/3. That late March interface is now buried 2 to 5 feet deep and is gaining strength. Future avalanche concerns are transitioning away from this specific interface, and back to more isolated areas that have a weaker-than-average snowpack. Areas with a relatively shallow snowpack will have more pronounced layers of facets that have developed throughout the winter. The most common areas to find these weaker snowpacks will be steep rocky slopes with variable snowpack depths, and areas where previous winds have eroded the total snowpack depth creating large fluctuations in that snowpack depth across the terrain. This video sums up an example of this type of terrain.
Avalanche crowns spanning steep, rocky terrain. This avalanche ran sometime during last weekend's storm.