Truly remarkable to have 110cm of snow on south-facing terrain below 6500'. There were 2 dust layers present in melt-freeze crusts below the recent storm snow which will have albedo implications when exposed in the next few weeks. Roughly 80cm of settled snow sits above 30cm of very large polycrystals formed during mid-march via pendular metamorphism. In this particular location, the storm snow was not highly unstable as its' structure was right side up and adhering well to the old MF crust. However, the wind was doing its dirty work and I suspect nearly all slopes NE-SE below ridgelines were both heavily wind loaded and sensitive to triggers today.