Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
The new snow from Saturday night was reported as well bonded to the rain crust. Signs of instability at mid-elevations were limited to small slabs and sluffing. It’s still worth investigating wind-loaded slopes - and all slopes at upper elevations - before diving into anything bigger or steeper.
You can use the rain crust about 10-16” down from the surface to track changes in new snow depth. More and stiffer snow = a greater chance of triggering a slab. Use a ski pole or simply dig down with your hand to find the crust as you gain elevation and change aspects. Look for instability using test slopes, hand shears, and other simple tests.
Choosing lower-angle terrain features, or slopes with no consequence in the runout below, are easy ways to reduce risk in avalanche terrain.
A human triggered slab avalanche from a prior winter.
Photo: NWAC Public Obs