Snowpack

Observation: Park City Ridgeline

GraingerSalt Lake
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Quick report

Red Flags
Poor Snowpack Structure
Red Flags Comment
<p>Aside from Low and South, things don't look good for future loads. Best will be to get a good look at the coverage and continuity of this trash heap snowpack in the days preceding our next snow.</p>

Deeper layers that looked strong a couple weeks ago are faceting and weak.

The most interesting example of the deteriorating mid-November crust I could find was ~9000' E-facing and was still 1F. Snow below and above had weakened significantly.

Snowpack

Traveled from Empire Pass area to Murdock.  Generally along the PC Ridgeline:

-Faceting is occurring in all snow that is not a crust.  Snowpack height is less than 60cm even on high protected slopes and the night temps are providing all of November's snow a faceting temperature gradient.

-While areas of the upper Cottonwoods still hold somewhat weak, rightside-up snowpacks, much of the N through E of this area is more faceted throughout.  Thinner HS has slopes that weren't wind-slabbed Monday night faceting to the ground ("Sandboxing" colloquially).  Full ski penetration on steeper pitches, just tip-toeing and hoping for soft shrubs underneath....

-The mid-Nov thermal crust is present but deteriorating on all but high northerly slopes.  I imagine this fully deteriorates soon with current weather.

-Southerly slopes continue to have their surfaces heated and cooled enhancing the already stout M/F crust.  Very thin, discontinuous snowpack on mid and lower elevations and all solar aspects are a layercake of crusts and further-weakening facets.