We skied the negatives and dream bowl, and noticed that there were sections of old wind board snow on east to north slopes, buried under varied snow depth. For the most part, the snow on top was low cohesion, but there was a low distribution of wind slabs across the north to east. That winds slab was soft but had higher cohesion then surrounding snow and produced shooting cracks by walking through it. The distribution was low, but sensitivity was fairly high, so we decided to turn around.