Old snow surfaces are a mixed bag of wind and melt freeze crusts, and both damp and dry soft settled powder. Supportable quasi - corn found on mid/low elevation sunny aspects. Last week's surface hoar appears to be long gone and any surface facets have been affected by warmth, wind, and direct sun.

Cool to find wind deposited surface hoar. See below - Interesting to note that one can - under certain conditions - have facet/slabs from wind blown snow (but surface hoar wind slabs? )

And the dramatic drifting over the past couple of days - note the wind feature pointing in to the wind (looker's left to right) in contrast to the cornice in the background leaning looker's left to the east.