Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
There is plenty of available snow for transport, and winds will build slabs on lee aspects at the highest elevations. On northerly aspects, these slabs have formed over weak snow grains. There have been avalanches triggered on this layer in the Darland Mountain area on wind-loaded eastern aspects at approximately 6800ft. Observations of avalanche activity suggest that the sensitivity of this layer may vary significantly throughout the terrain. Therefore, adjacent slopes may react differently, and it may not be the first person on the slope who triggers an avalanche. The best way to avoid being surprised by one of these avalanches is to stick to wind-sheltered areas or lower angle slopes in high elevation, northern and eastern aspects. Always look for signs of instability such as shooting cracks, collapsing, or recent avalanche activity. These are all bullseye signs of an unstable slope. You can also dig down quickly to observe if the snow slides easily off the crust and look for weak snow above the crust. If the snow easily slides on the crust, you find it weak snow, or see other signs of instability stick to conservative terrain with lower angle slopes.
(3/18/2022)
The crown from a recent snowmobile triggered wind slab that failed on the March 8th facets at approximately 6800ft on an eastern aspect.
Photo: Andrew Kiefer