Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Typically, by this time of year, we are getting close to putting our PWL problem in our rear view mirror. Unfortunately, we have a particularly weak and shallow snowpack this season brought on by few storms and long dry spells. Prior to the Valentine's Day storm, pretty much the entire snowpack was loose, weak, and faceted on slopes facing W-N-E. The Valentine's Day storm built a thick, dense slab on top of this weak structure creating one of the worst snowpacks I've ever seen. The Valentine's storm produced a few natural avalanches but not a widespread cycle and things were left hanging in the balance. The storm last week added a little more weight producing a few more avalanches including one very large, full depth release in Horse Creek. And here we are again. The underlying structure remains very poor and we've added a little more weight. The bullseye area for this problem is on steep, northerly aspects near treeline, and the likelihood decreases the further you step outside of this area. Personally, however, I'm going to continue to avoid any slope steeper than 30 degrees where this structure exists.
Ryan Huels performed an extended column test on a west aspect on Saturday and got a score of ECTP 23. We had similar results on Friday. Although stubborn, any propagation shows a propensity to avalanche, it's just a matter of finding the right trigger point. This could happen after one or many people have skied the same slope. It's just not something I'm comfortable messing with right now.