Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3
With the threat of very large natural avalanches largely behind us by Sunday, human-triggering remains a concern, particuarly at upper elevation. We're moving into a low likelihood, high consequence threat for very large human triggered avalanches. This threat mostly exists in large alpine bowls where intense winds overloaded start zones multiple times over. Given the size and consequence, it would be prudent to wait another day to test heavily wind loaded alpine bowls, chutes, and poorly supported rollovers. Seek less consequential, smaller terrain features once you ascend above the 3/14 maximum elevation of the 3/14 rain crust (likely around 6500 ft)
Observers reported shooting cracks, a sign of instabilities within the upper snowpack in wind-loaded areas around Pea Gravel Ridge. It is uncertain how long-lived this instability may be, but it's worth finding wind loaded test slopes where you can test for firm over weak layering or stomp on a poorly supported pannel of snow to see whether wind slabs continue to be reactive in your terrain. Be aware that with the strength of recent winds, slabs may exist well below typical start zones. Don't hesitate to seek trees or wind sheltered terrain if you are in doubt. A crust near the snow surface limits wind deposits to more manageable deposits or lens-shaped pillows that you can steer around at middle elevations.
(3/14/2026)
Shooting crack on a small slope test above a skin track.
Photo: Kyle Wyatt