Snowpack Summary
Wind slabs exist on slopes lee to the west. Below these surface layers, the snowpack is reported to be generally well-settled. Snowpack depth is below threshold for avalanches below about 1400 m (or as high as 1800 m on some slopes). Cornices have grown large in some areas.We are still watching a few layers, but recent snowpack tests have suggested that these are generally fairly well bonded. There is a buried rain crust in the upper snowpack which fizzles out at about 1800 m. A localized layer of surface hoar buried about 1 m down may still exist in sheltered pockets. At the base of the snowpack, a variable early November crust/facet layer exists. Any of these layers could become reactive with heavy loading, or if triggered from a thin snowpack area.