What we saw today was soft slab new snow avalanches failing on a density change within the newest snow and had to do with strong snowfall (precipitation) intensity. The density changes (heavier and lighter snow falling out of the sky) within the newest snow were the weak layers. These will typically settle out quickly, but if allowed to entrain a lot of the new snow they can be larger than you may expect particularly on steep long running slopes where snow can pile up on benches and in gully features. Today the tails of my skis were still hitting the melt-freeze crust in some locations, but the avalanches were failing on a density change in the recent storm snow above the crust.
Photo taken just before snowfall tapered off showing radar (band 13) with snowband (greens and blues)