Lawine

Avalanche: Park City Ridgeline

Park City Snow Safety/UACSalt Lake
Auf der Karte ansehen
Beobachtungsfoto 1

Quick report

Slope Angle
36°

Avalanche

Slab Width
91 m
Weak Layer
Facets
Vertical Fall
152 m
Avalanche Type
Hard Slab
Slab Thickness
122 cm
Start Zone Aspect
East
Avalanche Problem
Persistent Weak Layer
Start Zone Elevation
2957 m

The crown face on this avalanche was 2-6' deep with an average depth of 4'. The right and left flanks tapered down to 1'. It was estimated to be 300' wide and ran 500' vertically before stopping in the flats. This would have been an unsurvivable avalanche.

It was difficult to determine a trigger, however there were snowmobile tracks on the ridgetop adjacent to the slide. The crown spanned aspects from east- northeast and there was some variability in the hardness of the wind slab over the weak layer throughout the crown face.

The weak layer was approximately 80cm off of the ground and consisted of a very thin melt freeze crust with small grained facets above and below. There were sections of the bed surface that were over 1 meter deep. What this tells us is that the weak layer is elevated off of the ground. What this means for us as backcountry travelers is that the potential for much larger avalanches could be more prevalent this season.

This avalanche was reported late in the day on Saturday December 3, 2022. DPS did a fly by and worked with Park City Patrol to determine that there was no one involved. This avalanche occurred in closed terrain within the Park City Ski Area Boundary and resembles backcountry terrain in similar areas.

As you travel near ski areas please respect their ski area boundaries. Check out resort uphill policies here.

If you see or are involved in any avalanches around ski area boundaries please report them to the appropriate rescue organization.