Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Several waves of precipitation, fluctuating freezing levels, and strong winds have resulted in a layered upper snowpack. You’ll need to check the recent storm snow for weak interfaces and its bond to the old surface by digging. Small test slopes and uptrack tests won't cut it when the snow is this deep. Heavy snow over weak snow, layers of weak grains such as graupel, or wind-drifted slabs hidden below the surface are just some examples of potential failure points. Slabs should be larger as you ascend in elevation or in wind-loaded terrain. You’ll need to contend with storm slabs, wind slabs, and loose avalanches as you pick your way through the mountains. Regardless of the avalanche problem, you’re more likely to trigger one on slopes over 35 degrees.
In isolated locations, natural avalanches could still occur. We wouldn’t be surprised to hear of an avalanche stepping down into old snow layers and growing very large.
(2/28/2024)
Debris from a large natural storm slab reached down into the trees below the main bench of Kendall Peak. SW 5400ft SS-N-D2-R1-U
Photo: Dallas Glass