Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 4
You can still trigger deep and destructive avalanches 3-5'+ deep and hundreds of feet wide.
The most suspect terrain continues to be the west through north through southeast facing aspects at mid and upper elevations. HOWEVER, with the recent snowfall, the expected snowfall, and the increasing winds - I am worried that some upper elevation south-facing terrain and low elevation north-facing terrain will become active. I am not sure about timing, it could happen today, tomorrow, or even Wednesday - but the dangerous set up is there.
These types of avalanches are most pronounced in steep, thin rocky terrain...and areas that have previously avalanched this winter. They may be more prevalent along the Park City Ridgeline, Upper Mill Creek, Upper American Fork, and the Snake Creek drainages.
Keep in mind:
- Existing tracks on the slope offer zero signs of stability.
- Avalanches can be triggered from a distance or below.
- Any fresh wind slab or new snow avalanche may step down several feet into older snow.