The main hazards are rocks and other obstacles that aren't covered or barely covered by the thin snowpack. There may be some isolated, shallow slabs of wind drifted snow near ridgetops that could produce a small avalanche from increased winds two nights ago.

Otherwise, the snowpack continues to facet and weaken on most slopes except ones receiving direct sunshine. This faceting process occurs because the ground is always 32 degrees F and the snow surface is much colder which creates a big temperature difference over a short distance (because the snowpack is thin). To get avalanches, we'll need snowfall and/or wind to put a slab of snow on top of this weak snowpack.