Up to 65 cm of new snow (and an additional 15 cm by Wednesday afternoon) sits on a melt-freeze crust at treeline and below. New snow and strong winds will be promoting ongoing slab formation. The new snow may be sitting on a weak layer of surface hoar (feathery crystals) in sheltered areas.For most of the region, a weak layer of facets (sugary snow) buried in early December exists down 150-200 cm. It is likely that this layer was the culprit of a large, remotely-triggered avalanche on December 30 near Terrace, described in a MIN report
here. The likelihood of triggering this layer is decreasing, but it could be triggered by humans in shallow snowpack areas. The potential may also exist for storm slab avalanches to step down to this layer, resulting in large avalanches.In the northern part of the region, near Ningunsaw pass, a couple of weak layers of surface hoar may be found that were buried near the end of December. Expect to find these layers about down approximately 50 to 120 cm.