Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3.5
Two buried persistent weak layers could be potential problems as the new snow accumulates.
A weak layer from mid-February is likely down over 60 cm and may become more reactive as the overlying snow forms a thicker and more cohesive slab. Two weak layers of surface hoar from January are likely down over a meter and were primarily a concern in the east of the region on northerly aspects around treeline.
Storm slab and loose wet avalanches have the potential to step down to these deeper layers.