Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1.5–2.5
The recent snow loaded a weak layer of surface hoar crystals in some areas, which is at a prime depth for human triggering. The layer is most prominent in areas sheltered from the wind at and below treeline. Example terrain features to particularly treat as suspect include the lee side of ridges, openings in trees, cut blocks, and burns. Large, wide-propagating avalanches could result where this layer is present.
The buried weak layer was reported to be present up to treeline in the Torpy Sande and Pine Pass areas and in isolated areas in the Renshaw. Avalanche activity on this layer was reported in the south of the region.