On this prominent west aspect above Delia Creek, at 3600 feet, I saw the remnants of three old D2 Wind Slab/Cornice avalanches that occurred from strong east winds potentially after March 1. In at least two of the avalanches chunks of cornice were observed in the debris that were knife hard and 2+ feet thick. The avalanches all originated just below or at the north/south running ridgeline. From a distance the crowns appeared to be upwards of 3 feet thick and 100 feet wide. The two larger avalanches ran a distance of 600-800 feet in length, one of which filled-in some of a large terrain trap. I believe that these avalanches failed on a buried layer of facets below the wind firmed slab.