Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2–3
We have a layer of very weak snow (facets and crusts) buried in our snowpack. In this zone, it sits beneath a 3-4+' thick slab of dense snow that was built in the past 2 weeks. This weak layer has produced numerous large and very large avalanches already this season, including this slide on Galena Peak that was observed in a period of clear weather on Christmas Eve. Yesterday, in the Baker Creek drainage, I observed several large natural avalanches that had failed within the past day (photo), and riders reported experiencing a large snowpack collapse that they could feel while they were on their machines. This weak snow is preserved on middle elevation slopes on the shaded (north) side of the compass and on most slopes at upper elevations. I made a video yesterday to try to help explain where you will find this snow and why that is important, you can watch it here. I think it is worth your time.
Weak layers like this are hard to deal with. They behave in ways that tend to catch even very experienced backcountry travelers off guard. Avalanches can be triggered remotely, from long distances below, above, or to the sides of steeper slopes. Avalanches that fail on this snow may pull back into gentler terrain above steep slopes thanks to the very dense slab of snow. Any avalanche that breaks on this weak snow will be very large, and likely unsurvivable. We are less than 24 hours out from the last snowfall, and this weak snow has hardly had time to start adjusting to its load. It won't take much to push it to its breaking point: that could be a collapsing cornice, a wind slab, or you.