Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 2–3
The official seasonal transition to spring arrived on March 20, and the mountains just received three to four feet of snow since. This amounts to a broad brush 4 to 6 inches of SWE in the past four days. This substantial new snow volume and water weight has built dense, cohesive slabs across all aspects and elevations. These slabs now sit atop more storm layers that formed between March 12 to 18.
The most recent load is placing significant stress on a variety of interfaces (hardness changes, subtle grain type differences, and crust) in the upper snowpack, with stability teetering near the edge. Steady elevated wind speeds have also been effective at drifting the denser snowfall into deeper drifts or slabs below leeward-facing ridges and gullies.
(3/16/2025)
Looking across the right flank of a skier triggered slide on an east-facing slope around 6400 feet. The slide broke over 300 feet wide and around 2 feet deep, and likely failed at either a recent storm interface or in softer snow above a sun crust. Blue Mountain, Selkirk Mountains. March 16, 2025.
Photo: Chris Bilbrey