Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Although limited, our data for the zone shows that this problem has trended toward unlikely. That being said, there is uncertainty about how wet buried weak layers 1-1.5 deep in the snowpack are, and if some reinvigorated instability exists. Rain has fallen at upper elevations near the Cascade Crest and will continue to do so at least through Sunday morning. Areas to the east of the zone have wet snow, too, thanks to very warm temperatures and sunshine. You can dig in and see how far down the snow is wet within the snowpack. If you can easily make a snowball with a gloved hand or even squeeze water out, that snow is not dry.
The most suspect place you'd still trigger a slide is in exposed wind-loaded terrain, and weak layers can be buried even deeper here, too. Falling cornices in these areas could be just the big trigger needed to let loose a deadly avalanche. As freezing levels drop throughout the day and snow begins to fall at upper elevations, small wind slabs may also form in this same terrain.
This problem is tricky to manage in the backcountry, especially when it's unlikely, but not impossible, to trigger a slide. If you plan to travel near a neighboring forecast zone, consider reading that forecast as well to equip your toolbelt with more information, given the limited data for East Central. Either way, ease into steeper terrain and be thoughtful about the complexity and exposure of slopes you plan to ski or ride. You're unlikely to get clear feedback from the snowpack before triggering a large slide in consequential terrain.
(3/6/2026)
A snowpit dug recently on an east aspect at middle elevations in East Central. The upper snowpack and buried weak layers were already moist on this day, and are likely even more so on Sunday. Although the weak layers were healing, liquid water introduced to these layers could reinvigorate instability.
Photo: Payton Schiff