Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
A few large slab avalanches occurred with triggers in the West North Zone on Tuesday, with conditions similar to what you might see in the northern half of the West Central Zone. There were also a few storm interfaces noted around 6 inches and a foot down, but they are expected to heal quicker than the deeper avalanches. The deeper avalanches occurred just above a crust, probably involving a weak layer. This problem is not easy to identify and avoid. We currently know little about it after the large storm which just deposited 3 feet or more of snow at upper elevations.
You're most likely to trigger one of these large, deadly avalanches in the upper portions of near treeline and above treeline areas. Expect them to occur on large, steep, unsupported slopes. Until we know more about this weak layer, consider avoiding these unsupported slopes at angles greater than 35 degrees. An unsupported slope refers to a slope that rolls over into steeper terrain, without an abrupt transition to lower angle terrain under the steep rollover within a short distance. Pay attention to the usual signs of unstable snow such as cracking and whumphing, but these indicators are probably not precursors that you will find before triggering one of these deeper avalanches.
(3/15/2022)
An large slab avalanche which was triggered in the West North Zone on Tuesday.
Photo: Adam Ü