Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
A curtailment of wind activity will keep slopes from experiencing additional loading and warming temperatures will aid in the settlement of the snowpack. A natural avalanche cycle that resulted from wind loading has clearly identified where this problem may still exist. Multiple avalanches were observed on south and east aspects above treeline. These locations all share similar characteristics of being near or below catchment features and having a steep, convex slope shape. Be cautious if traveling among such terrain, as isolated pockets may still exist. Cross-loaded terrain on south and west aspects should not be overlooked.
(1/14/2024)
Casaval Ridge avalanches. East aspect at 9,400. SS-N-D2-R1
Photo: Eric Falconer