Snowpack depths at 8800-9000' were roughly 175-200cm and the snow was mostly* stable. (Repeater avalanche terrain and new wind drifted snow terrain not withstanding). Pools of graupel may also exist in usual terrain but I would imagine these would be increasingly difficult to trigger unless another significant load (cornice fall, another avalanche, etc). Otherwise I didn't see anything in the top meter that alarmed me. Uncertainty exists around the Valentine's Day facet/crust layering on east/southeast up high, but this - at least at many mid/low elevation areas - is well protected by a supportable or mostly supportable mf crust on the surface.

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• On solar aspects, I did not see any new radiation recrystallization facets above a crust. I would imagine the new snow coming in warm might bond favorably to warm and corrugated melt freeze crusts and/or damp snow.
• On polar aspects, it appears that very warm temperatures, cloud cover and wind has eroded, baked, or softened (rounded) the rough edges of the weak snow at the surface. The 3-4mm surface hoar has "baked in" via melt/freeze and/or is now "laying over". In general, "laying over" surface hoar is not as collapsible as it is when it is standing up and not as much of an issue. At least this is my experience.

Nature shot -