Overlaying slab is now a meter deep in many high elevation areas in upper BCC/LCC and consequently difficult to trigger. More than one interface facet layer could act as a failure layer. From the surface the snowpack appears more stable than it should be trusted due to a capping effect of the slab and dense, smoothed out graupel surface. Thin spots in the slab and large triggers could easily bring down large well connected slabs potentially running long and far. Remotely triggering an avalanche remains a distinct possibility.

Winds were still up for much of the day and snow transport was observed as low as the Brighton parking lot. Winds eased mid afternoon but will only add to the cohesively of slabs along ridges.