Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2
In areas closer to the Cascade Crest that have received more than 1 foot of new snow and counting, you could trigger an avalanche that fails on weak layers below. Slabs could be particularly sensitive on rollovers or convexities or where the wind has made them deeper and denser. This type of avalanche can break in surprising ways, wider than expected, and from flat terrain. It is unlikely that you will trigger an avalanche on south and southwest aspects, but we lack the certainty to completely rule it out right now.
Pay attention to the depth and cohesiveness of the surface snow. This will help you determine how much new snow there is as well as if the snow has been wind-affected. Cracking, collapsing (whumpfing), and recent slab avalanches are clear indicators that instability exists. Rippled, uneven snow surfaces and blowing snow will point you toward wind-loaded slopes. Ultimately, persistent slab avalanches are tricky to manage; your best bet is to just stick to low-angle terrain free of overhead hazards.
(2/1/2025)
This intentionally triggered persistent slab in the West South zone propagated the entire width of the feature. It failed on facets over a thin crust. ENE, 6200ft, SS-ASc-D2-R3-O, 20-24 in deep, 200 ft wide.
Photo: Dallas Glass