Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Where October snow lingered through November's warm temps and dry weather, it turned into a mess of slick crusts and sugary facets. This old snow is now buried beneath a dense slab that's 3' thick or more on most mid to upper elevation shady slopes. The weak layer in this zone is becoming more deeply buried, making it more difficult to impact with our weight. As a result, you're likely to experience less obvious signs of instability, but the flip side is any slide you trigger is likely to be a big one.
While the stability is (very) slowly improving, most observers are still reporting poor snowpack test scores. We're only about four days out from the big storm, and dribs and drabs of snowfall along with periods of wind transport are not giving the snowpack the break it needs. In short, the snowpack needs more time to pull it together.
While we've shaded the problem rose above to depict where you're most likely to trigger an avalanche, any slope harboring old snow (appearing as a mix of facets and/or crusts near the ground) is suspect. The difference between slopes that has old October snow and those that don't is fairly stark (watch video at right/above). Folks are finding safer avalanche conditions on low and middle elevation slopes that are southerly-facing and hence lack the old October snow.