Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Layers of weak snow can be found throughout the snowpack:
- Periods of sun, warm temperatures, and rain created a variable mix of crusts and facets near the snow surface. These crust + facet layers may produce smaller but touchy slab avalanches as snow accumulates.
- 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.
- Depth hoar exists near the ground on all aspects that hold snow. This is the weak snow that we've been talking about all season long and seem destined to talk about for the remainder of the season.
Ben found ugly snowpack structure and poor snowpack test scores near Dollarhide Summit (observation, photos) and in Adams Gulch (observation) 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.
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.