Avalanche

Schuylkill Ridge

Zach GuyGunnison
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Observation photo 1Observation photo 2

Quick report

Cracking
isolated

We traveled exclusively below treeline.  The new snow lacked much cohesion, and in steep terrain, was typically disturbed by some amount of overnight sluffing, slumping, or slabbing. By the time we got there around 9:30 a.m., the snowpack was quiet underfoot and we skied a dozen short, steep pitches with minimal signs of instability.  The underlying snowpack lacks much of a midpack.    It felt as if you found a steep slope where the new snow was undisturbed, with just the right ingredients of very weak facets underneath, you could trigger a slab in the new snow here, or if wind drifting increases tomorrow. We chose to avoid the bigger, higher-elevation terrain, where slabs might be more cohesive and entrainment potential more serious. 

One terrain feature produced shooting cracks up to 10'. Otherwise no signs of instability except for activity that ran overnight.

Weather

Cloud Cover
overcast
Wind Loading
none
Rain Elevation
N/A
Recent Snowfall
32 to 42
Snow Avail For Transport
large amounts

Measured 13" at 9000' and 16" at 10,000'. About an inch of snow fell during the day.

Snowpack

Ski pen is up to 60 cm: half very low-density new snow, half low-density facets above the Christmas Crust.  

Avalanche

Size
D2
Type
SS
Count
5
Aspect
E
Trigger
N
Elevation
11100 ft

There was a cycle of small (D1) storm slabs and sluffs that ran during the heavier precip rates last night on north to east terrain where we traveled. One in Climax Chutes grew to D2 in size, due to significant entrainment in larger terrain.