Snow surface is quite the mixed bag. Stout surface refreeze crust at low elevation yielded to softer conditons into the mid elevations. The northern quadrant of the compass at mid elevations no longer has the subsurface crust, meaning dense recycled powder (facets) all the way down. When it was possible to find sheltered terrain, this made for soft turns. Wind affected surface snow began around 7600ft, with the occasional 2cm wind skin fracturing a bit directly underfoot. Above 8300ft or so, most snow was either wind affected or scoured. From the saddle to the summit, the surface was either sastrugi or exposed bullet crust. By mid afternoon, low elevation snow was getting warm and slushy.