Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Multiple large to very large persistent slab avalanches were remotely triggered in this zone on Friday and Saturday (photo at right/above, video here). Slides occurred above Trail Creek, the East Fork of the Big Wood River, and near Baker Creek. These avalanches failed as dense, 2-3 foot thick slabs of snow. The culprit weak layer in these slides was the impressively widespread and fragile snow that developed during the December drought. Dig down and you'll find facets and/or surface hoar on shadier aspects and crust + facet combinations on sunnier slopes.
Triggering similar slides is likely again today. You can trigger avalanches that fail on these weak layers from long distances away from steeper slopes. Some of the triggered slides from the past two days released over 1,000' away from where the slope initially collapsed.
The recent snow is adding significant stress to the persistent weak layers in the snowpack, and represents the first major loading event that large portions of this zone have experienced. The recent triggered slides clearly indicate that the snowpack is not reacting well to this loading. Pay attention to the terrain you are in and the terrain you are exposed to from above.
This large remotely-triggered persistent slab avalanche on a NE slope at 9400' above the East Fork of the Big Wood broke 250 feet wide and ran over 1000' downslope.