On protected slopes around 6 inches of snow sits above settled snow from storms on the 11th and 13th. Snow since the 11th totals around 13 inches in this area. On east slopes, a thin melt freeze crust separates recent snow from weak 2-4 mm facets (F-) to the ground. We received a collapse in the area we dug along with moderate propagating results below the crust.
We also dug in a cross-loaded feature to assess instabilities related to the rapid wind loading. This feature held a connected base of facets formed during our long drought period. A variety of wind-packed layers divided by softer snow makes up a thick slab of all the snow drifted and cross-loaded since the 11th. Impressively this recently drifted snow has formed a slab nearly 75 cm thick making up more than half the snowpack in this area. We received moderate propagating results below this slab at layers likely relating to 2/11 and 2/16.
With strong winds continuing through this storm we can expect to see rapid loading on lee slopes and cross-loaded terrain features that will form a deep connected slab sitting on a bed of marbles.