Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
The outlier. I suspect that the Mill B South avalanche is more the exception than the rule but I feel it probably involves a facet/crust structure from last Wed/Thurs. While nearly everything else in the range was skiied/ridden with impunity the last two days, this avalanche warrants great attention and respect. East to south to west facing slopes must be investigated individually to determine if this unstable layering exists as cracking and collapsing may not be present.
Again, these are unusual avalanches on unusual aspects for us here in the Wasatch.
Thanks to those who went out yesterday actively digging on these aspects (Gagne, Paradis, Catino and others). As you'll read in their observations, nothing they found provided any indication of unstable layering that would avalanche.
Hopefully we will have this avalanche investigated today.