Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
This zone has persistent weak layers buried 1-3 feet deep on most middle and upper elevation slopes. Recent observations from this zone indicate that these layers are trending towards "dormancy", and fewer signs of instability are being reported. But an observer in the mountains east of Hailey experienced a snowpack collapse that caused an area 50 feet in diameter to crack around him. This is a good reminder that our weak layers of facets, depth hoar, and surface hoar still lurk in the snowpack ... #stillthere.
Today's forecasted 2-5 inches of new snow will not significantly impact these layers, and we remain in a holding pattern. You can reduce most of the risk of triggering a slide by understanding where avalanches remain possible and avoiding terrain with these characteristics:
- Wind-loaded terrain: Slopes where recent or past wind formed drifts and/or stiffened the snow surface. This is especially true in the Wood River Valley, where many wind-sheltered slopes are turning into full-depth sugary snow.
- Steeper slopes: "Prime-time" avalanche terrain around 35-45 degrees in steepness.
- Southerly facing terrain: In the Soldiers where there is more consistent snow coverage on sunny slopes, crusts and facets 1-3 feet deep seem to be stabilizing more slowly than the weak layers on shadier slopes.