We observed two crusts in the snowpack. One below our recent snow from last week's storms (late-January crust) and the curst from early-December's rain. Recent snow above the late-January curst is faceting with clear skies, cold temperatures, and falling winds.
We suspect this crust may make it less likely to trigger avalanches on the facets above the early-December curst at treeline, but we expect it is less prevalent in the alpine. It likely does not exist on alpine northerly aspects. We will continue to investigate the distribution of this newer crust and how it may influence the likelihood of triggering avalanches on the early-Dec layer.