Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
We currently have a snowpack structure primed for avalanches: the classic strong-over-weak setup. It’s a tenuous balance, just waiting for enough new snow and wind to tip the scales. The key questions are whether the storm delivered enough of a load and if avalanches will be triggered today.
Given the storm totals nearly 2' in some places and sustained high winds, the answer is likely yes, but primarily in areas that receive the most snow and wind - read, upper Big Cottonwood, Park City Ridgeline, areas of the Wasatch back that had snow on the ground prior to this event. Expect to trigger 1–3' deep soft slab avalanches on slopes facing west to east at mid and upper elevations. These slabs will likely fail within the old snowpack—a mix of weak, sugary facets and crusts. In steep, wind-drifted terrain, watch for shooting cracks, audible collapses, and the potential to trigger soft slabs.
Listen for whumphs or collapses, test small slopes to gauge reactivity, and look for shooting cracks. Extended Column Tests can also provide valuable information about snowpack stability. Proceed carefully and be prepared for reactive conditions.