Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
A significant amount of snow transport was observed on Mount Albert on Friday, which means that the wind slabs present in the mountains on Saturday will have formed within the last 24 hours and are therefore likely to still be unstable.
They are found mainly beneath alpine ridges and in areas of lateral loading at the tree line. These slabs rest either on a crust or on a thin layer of ice pellets, sometimes both. These interfaces provide excellent gliding surfaces for avalanches and make them easy to trigger when a skier passes over them.