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 settled or has been wind-affected. Cracking, collapsing (whumpfing), and recent slab avalanches are clear indicators that instability exists, but you might not see any before it's too late. Rippled, uneven snow surfaces and cornice development 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.
(2/3/2025)
A skier triggered persistent slab avalanche near White Pass. This slide released over a 100ft wide and 2-3ft deep. WNW, 5600ft SS-ASu-D2-R2-O