I traveled around the lower ends of Lake, Rolfson, Staker and Miller Flat Reservoir.  White out conditions prevented me from getting into the upper portions of the drainages.  I quickly found weak snow near the rain crust which is buried around 85cm deep.  In areas that had a total depth of around 180cm the weakness was more pronounced then in areas that are deeper.  The weakness is stubborn but no doubt present.  A significant new snow load with wind transporting it along with a trigger such as a sledder could trigger deep and dangerous avalanches on the more northerly facing slopes.

The photo shows the weak grains present at the failure under the rain crust.  Mostly faceted grains but surface hoar still present as seen right in the middle of the photo.