Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Storm slabs may be easily triggered on Saturday, especially first thing in the morning. Look for signs of instability like cracking and recent avalanches. Slabs could fracture wider than anticipated if they fail on layers of buried surface hoar, facets, and/or a thin crust from earlier in the week. Avalanches could become 1.5ft deep, especially in areas of wind loading like near ridgelines. You can use test slopes to check and see how upper layers are reacting, but it's not the day to trust many steep slopes. Buried surface hoar is 'spatially variable' in that you may not find it 7 times out of 10, but those 3 times, well...
We also have some uncertainty with deeper layers of the snowpack above 6,000ft, and on the eastern edge of the zone. Here, more snow may accumulate, further stressing these layers.
Example photo of a small storm slab.