Most slopes have entered a
daily melt-freeze cycle, with the exception of north-facing terrain above 1800 m. On these colder slopes, you may find 10-20 cm of powder or isolated wind slabs. These same slopes may also have a layer of faceted grains buried 50 to 70 cm below the surface, but this layer has shown signs of strengthening. Elsewhere, the surface has been melting each day and then freezing into a hard crust overnight. Snow is disappearing rapidly at lower elevations.