There is weak, sugary faceted snow (a persistent weak layer, or PWL) on almost all aspects and elevations throughout the Wasatch Range. This PWL has been buried by several feet of storm snow and wind-drifted snow which has created dangerous avalanche conditions, with three serious avalanche accidents this past week. WHAT IS UNUSUAL is that each of these avalanche accidents took place in the lower elevations bands below 8000’. What this means is that these avalanches can occur not far from parking lots or trailheads.This PWL is especially dangerous on aspects facing northwest through north and east where triggering avalanches is likely.

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Northwest winds overnight have had plenty of low-density snow to blow around and you are likely to find sensitive slabs of wind-drifted snow at the upper elevations. The new soft slabs will be most pronounced on north through east through south facing slopes. The avalanche in Snake Creek on Thursday likely failed due to recent wind loading and there were other reports of sensitive wind drifts from Thursday.

Any wind slab avalanche that you trigger has the potential to step down into deeper weak layers in the snowpack, creating a very large and dangerous avalanche.

Look for evidence of fresh drifts and wind slabs that look wavy, rounded, smooth, and pillowy, and avoid those slopes. Signs of sensitive wind-drifted snow include cracking and collapsing of the more dense drift over lower density snow below.