Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
To get an avalanche, you need three things working together: a weak layer, a slab on top of it, and a slope steep enough to slide. Right now, we have all of that, with old October/November facets buried under recent storm snow on slopes steeper than 30 degrees across the northern half of the compass.
We saw plenty of proof over the weekend, with widespread avalanche activity and obvious red flags. As we move farther from the loading event, those signs might not be as obvious, but the dangerous setup is still very much in play.
This extends through both upper- and mid-elevation terrain, and both should be approached with caution, though upper-elevation slopes are the most suspect today. These areas received the most snow and have the most connected weak layer. Avalanches in this setup can even be triggered remotely, meaning you could collapse the weak layer and start a slide from a distance.
Yesterday, I went to check the slide Trent and Brooke remotely triggered on 12/6. It broke roughly 1-2 feet deep, spanned nearly 200 feet, and was powerful enough to bury or injure someone. Check out my video BELOW.