Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Soft slabs of new and drifted snow averaging 1 foot thick will be most sensitive to triggers where they formed over fragile facets, collapsible crusts, or surface hoar layers on west, north, and east aspects. Slab behavior is becoming more challenging as slabs thicken from windloading and snow, with increasing potential for remote triggers and wider propagation around terrain features. On these same aspects at mid and low elevations, avalanches will grow larger as they entrain the weak, sugary snowpack under the new snow. Cracking and collapsing are warning signs to travel on slope angles less than 30 degrees.
Older, hard slabs exist below the storm snow on some leeward slopes and can produce avalanches that are more surprising or difficult to manage. Identifying the locations of these older slabs is now challenging beneath the new snow.
A skier triggered slab avalanche that broke on weak facets and gouged to the ground above the Slate River on 12/27.