Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
You can trigger large, dangerous avalanches on just about any steep slope you encounter. Yes, even at lower elevations and in terrain sheltered from the wind. Widespread weak layers are now buried beneath 1.5-3 foot thick slabs. This combination produced a remarkable avalanche cycle in this zone last weekend, with avalanches likely numbering in the hundreds.
In the past two days, I've experienced very large, booming, rumbling collapses in different portions of this zone. I could feel the snowpack drop beneath me when these happened, and watched as snow rattled off of hundreds of trees over large areas. Yesterday, a public observer reported seeing a relatively recent avalanche that had been triggered by an animal. These are obvious signs of instability that should not be ignored. Tilt these collapses up onto a steeper slope and you have yourself an avalanche.
Persistent weak layers produce avalanches that behave in surprising ways. They can break wider than you'd expect and can be triggered remotely—from gentler terrain above, below, and to the sides of steep slopes. Plan your day expecting to be able to trigger these types of avalanches. Thanks to the widespread nature of the weak layer+slab combination, avoiding slopes steep enough to slide is the only way to ensure a safe return home. Playing on or below steep terrain continues to be a risky dice roll.
(12/13/2022) Numerous large avalanches were observed in the Lake Ck Drainage N of Ketchum. This large avalanche is on a NW-facing slope at 8,400' near Triple Pk.