The total height of the snow is around 120cm. The top 20cm is low-density, accumulating storm snow, falling on 2 to 10cm of very weak near-surface facets. The only real structural integrity is a 60cm-thick 1F slab, split in the middle by the Christmas facets (we were above the crust line at 11400 feet). Below the mid-pack slabs are weak, large, large-grained facets to the ground. Avalanches could step into the Christmas layers or the basal facets; both layers were unreactive in snowpack tests and showed signs of strengthening. That said, this ongoing rapid, substantial load could be enough to trigger deeper breaking avalanches.