Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible - Likely
- Tamaño
- 2–3.5
Weak layers from February (mostly crusts and surface hoar) are likely down around 60 cm and may become more reactive as the overlying snow settles into a denser slab. Two weak layers of surface hoar from January are likely down 100 cm or more and are primarily a concern in the east half of the region on northerly aspects around treeline.
A 1-5 cm thick crust that formed in early March could make it more difficult to affect these layers with the weight of a human or snowmobile, BUT if you aren't feeling the crust underneath you, or if you feel like your turns are digging in below it, choose simpler terrain and give avalanche terrain a wide berth. Remote triggered avalanches have been recently reported on this layer.
Diligent terrain selection is required for this type of avalanche problem. Signs of instability may not be visible on the surface, and the resulting avalanches will be large. An important part of your strategy would be to avoid rocky start zones below ridgetops and convex rolls.