Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Enough new snow should accumulate at middle and upper elevations to pose a real hazard. There are three questions you can ask to help determine how likely you are to trigger an avalanche.
- What did the snow fall on? Dig down with your hand as you travel. The new snow should bond well to the underlying wet snow. Once frozen, this often presents as a crunchy crust. If the new snow sits on a layer of ice (freezing rain), it may slide off very easily.
- Is the snow influenced by the wind? Look for clues like blowing snow, drifts, or firmer slabs. These wind-loaded areas could produce larger and easier-to-trigger slides.
- Are there layers within the new snow? Weak layers can form within the storm from changes in precipitation rate, temperature, or even snow crystal type. Hand pits, uptrack tests, and small slopes can all highlight inter-storm layers that are more likely to slide.
Given the dynamic nature of this storm, you could encounter plenty of spatial variability. Make frequent observations that can tip you off to more likely avalanches. In these spots avoid steep, open slopes.
(2/28/2024)
Example: You can use uptrack tests like this to check the old/new interface.
Photo: Dallas Glass