The snowpack structure is fairly complicated right now. A PWL (persistent weak layer) of faceted snow is buried 1-2' down. Below the post-Christmas storm lies a very slick and - in many areas - very thick (up to four inch thick) Christmas Eve rain crust (CERC) essentially capping the poor structure below. The structure has shown its cards, however, as a skier triggered a 2-3' deep and 70' wide hard slab on Sunset Peak in the Alta/Brighton backcountry on Sunday and a similar avalanche ran naturally beneath the Twins of Snowbird just down the street that same morning. Explosive control work pried out a couple similar hard slabs in nearby terrain that same day.
We've heard of nothing since. And nothing in the Provo mountains.
So what to make of it? I think it would be pretty difficult to find a place to trigger one of these hard slabs, but not impossible. If you were hunting, you might find trouble in upper elevation, thin, rocky terrain where the rain crust is thinner. The rain crust that collapsed on Sunset was only one inch thick (see Dave Kelly's excellent report HERE).
Photo of the Sunset avalanche from Sunday below. Note this avalanche was on very steep north facing terrain at 10,400'.
