Snowpack

Below right gully @ 4700'

Avalanche.org observerPresidential Range
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Observation photo 1Observation photo 2

Quick report

Cracking
specific
Collapsing
isolated

Where the skiing looked good (in the more sheltered, non scoured areas we travelled through) we observed multiple signs of instability in the snowpack between the new snow-crust interface including cracking and whumpfing. We were quite content not traveling in or skiing anywhere steep + connected enough to slide. Noticed cracking in the upper layers of the snowpack while skinning up. Snowpack collapsed with a big whumpf while we were transitioning beneath the buttress.

Weather

Air Temp
5
Cloud Cover
clear
Wind Loading
light
Recent Snowfall
14 cm
Snow Avail For Transport
moderate amounts

Snowpack

Snowpack consisted of areas of scoured crust that was barely skier supportable (not boot supportable) and areas of 1-4F windslab on top of the crust. The windslab was more widespread than the exposed crust. We dug a mini pit where we transitioned at 4700' where we observed 40 cm of 1-4F windslab on top of 4 cm of 2mm graupel lying directly above a P hard crust. Beneath the upper crust were a series of other crust/ice layers. A shovel shear test collapsed upon isolation (STC) on the graupel layer (see photos). We guessed the whompf we heard to also have been a collapse on this layer.