Wet snow issues will persist for the next few days until the next storm. There has not been enough transition to spring weather and therefore the upper 2-3' of snow has various crusts, grains and degrees of cohesion...and avalanches will continue to be possible until there is a proper melt-freeze regime. As such, we noted collapsing in the superficial crust on less cohesive wet grains below (lower elevations). An ECT revealed ECTPs a foot down at a crust/loose wet grains interface. Very easy to see "strong over weak" and/or hear collapsing in the snowpack.

That said, timing. is the name of the game in the spring - two skiers had skiied off the summit of Ben Lomond down the headwall by mid-morning.

We noted many many natural soft slab avalanche pockets in, below, and south of the Bailey Spring area on east/northeast facing slopes in the mid and upper elevations, well off the ridge-lines and at terrain features. These most likely ran Sunday with the higher winds.