Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
You're more likely to trigger generally small (up to size 1.5) slabs formed by the more recent round of wind NE wind in locations. These slabs should be confined to the snow above a density change formed by winds over the weekend. Pay attention for signs of wind transport near atypical S and W aspects. Some of these slopes melted to bare ground and rock and have shallowly submerged sharp objects that will increase the trauma from any avalanche.
Don't let down your guard if you find less wind-affected snow on the surface. Older slabs up to size 2 from winds over the weekend may be masked low-density powder. They should be stubborn to trigger and isolated to heavily wind-loaded, steep, and unsupported N and E aspects. Given the complex wind patterns, make sure to test for hard over weak snow layers all the way down to the 2/19 crust. When in doubt, stick to smaller terrain features and lower slope angles if you ascend into wind-affected snow.
(2/22/2022)
Explosive triggered wind slab (D1.5) in Heather Canyon. Failed within the storm snow.
Photo: Andrew Kiefer