Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
A mix of buried persistent weak layers makes for a complex and variable problem. Avalanches failing on buried facets are more likely in thin, rocky areas and terrain that slid earlier this season - referred to as repeater slopes. These facets near the ground were responsible for the recent avalanche on Ant Knolls in the Northern Provo Region.
We're also seeing avalanches breaking at the new/old snow interface, acting more like persistent weak layer avalanches in the mid-elevations. In some cases, the only way to identify this weak layer is by digging and performing a stability test. If you hear collapsing on any aspect or elevation, it's a clear red flag—stick to lower-angle terrain.
This buried weak layer isn’t done yet. Late February usually brings a shift in mindset toward spring conditions, but this season is different. Give the snowpack time to settle.
Video (Drew and I) discussing the recent rider triggered persistent weak layer avalanche from Ant Knolls.