Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2.5
Snowfall (1.3-1.5" SWE) and steady winds since Valentines Day have built and sustained cohesive slabs on top of an otherwise weak, faceted snowpack containing depth hoar and faceted crusts that formed during extended drought periods. North and East aspects contain the most abundant weak snow, in addition to the typical West-facing terrain along the Fraser-Wheeler ridgeline. Take the time to dig down in the snow to see if this strong over weak snowpack structure exists on slopes of interest. Multiple human-triggered and a few natural persistent slab avalanches have occurred over the last few days on these weak layers, which will continue to drive dangerous avalanche conditions today. Expect these avalanches to break deeper and wider in the snowpack as you move up in elevation, and in some cases near the ground, where they'll take will take with them most of the season's snowpack.
Loud audible collapses and shooting cracks mean that you've found this strong over weak snowpack structure. These conditions lend themselves to remotely triggering avalanches. Avoid being underneath steep slopes above, as it's possible to trigger avalanches from long distances away.
East aspect near treeline. The crown of a persistent slab avalanche (D2) that was easily triggered from walking along the adjacent ridgeline.
Photo: Charlie Harrison (02/19/2025)