Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely - Possible
- Size
- 2–3.5
Persistent weak layers could be potential problems as the recent snow settles into a denser slab. A 1-5 cm thick crust that formed in early March is making it more difficult to affect these layers with the weight of a human or snowmobile. Use extra caution if this crust is not present, or is breaking down due to warming from the sun.
Weak layers from February (mostly crusts and surface hoar) are likely down around 60 cm and may become more reactive as the overlying snow has formed a thicker and more cohesive slab. Two weak layers of surface hoar from January are likely down around a meter and were primarily a concern in the east of the region on northerly aspects around treeline.
Avalanches that start in the recent snow have the potential to step down to these deeper layers.