Wind loading patterns are very tricky.  Since there was only a couple inches of graupel to blow around when the huge winds blew a couple days ago, the wind slabs are subtle and mostly shallow.  They are more difficult than usual to see with surface clues.  Sometimes you don't know you are on one until you feel the hard surface and hear the hollow sound.  Luckily, there is a distinct dust layer on top of the rain crust so the darker areas are wind eroded and the white areas are wind deposited.

I did not see any clear evidence of avalanche activity during the storm.  There were some places that looked suspicious that a thin slab may have pulled out but the wind was so ferocious during the storm that it may have filled things in as fast as they released.