Manto nevoso

Hillman’s (Historic Runout area)

Ryan DeLena / Lucas RobdauPresidential Range
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Quick report

Cracking
isolated

At our targeted site we observed initiation and propagation on a layer of fist hard precipitation particles 45cm below the surface. This layer appears to have been buried by firmer wind slabs as wind speed increased during the storm cycle. Intense blowing snow obscured the upper mountain and we did not venture higher in Hillman’s or the bowl, so we did not observe terrain more exposed to the wind, but the snow surface at our test site is likely not representative of snow higher on the mountain. Still, this strong over weak structure is a good data point and something worth targeting for observation higher in the terrain when conditions allow. We observed cracking on a small test slope in Hillman’s historic runout. See photos.

Weather

Air Temp
-4
Cloud Cover
few
Wind Loading
intense
Rain Elevation
N/O
Recent Snowfall
None
Snow Avail For Transport
none

Sky Condition: FEW, Air Temp -20 C, Wind speed/dir: S-X, BLSN: I, New Precip: None

Snowpack

Snow depth: 290cm 290-260cm 1F 0.1mm DF 260-250cm 4F 0.5mm DF 250-240cm F 1mm PP (LOC) 240-185cm 1F 0.5mm DF 185-175cm 4F 1mm FC 175-150cm P 1mm ? 150-145cm IFil 145-0cm N/O CT6 SC Q1 down 45cm on F 1mm PP CT11 SP Q1 down 45cm on F 1mm PP ECTP16 down 45cm on F 1mm PP PST45/100END down 45cm on F 1mm PP