Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Layers of weak snow can be found near the ground and in the middle and upper portions of the snowpack:
- Depth hoar exists near the ground on all aspects (excepting low elevation slopes that are snow-free). This is the snow that we've been talking about all season long and seem destined to talk about for the remainder of the season.
- In the middle of the snowpack, several interfaces have produced both avalanches and unstable test results in recent days. These layers appear to be problematic where accompanied by a crust.
Ben found ugly snowpack structure and poor snowpack test scores near Dollarhide Summit (observation, photos) and in Adams Gulch in recent days. He also found a large, natural avalanche that appeared to have failed on a crust before stepping down to weak snow near the ground. This slide was located in exactly the type of terrain that still has me spooked in this zone: wind-affected slopes steeper than about 35 degrees. You can greatly reduce your risk of triggering a large persistent slab avalanche by playing on slopes less than 35 degrees that are sheltered from the wind.
(2/12/2021) This avalanche was triggered by a rider NE of Wells Summit in the Soldier & Wood River Valley zone. The slide broke around 40' wide and carried the rider about 100 yards. A section of the cornice also released in the slide.