Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 2–3
The persistent slab avalanche problem is trending in the right direction as we haven't seen these layers producing avalanches outside of one isolated avalanche in below treeline terrain. Faceted crusts from the end of February and early March dry periods are now buried 3 to 6 feet down in spots and would be difficult to trigger on your own but continue to remain present on slopes. It's most likely going to take an avalanche on the surface to step down into these deeper buried weak layers to get this layer to fail.
Below these layers depth hoar and facet layers from January continue to remain present in areas where the snowpack was shallow before this last storm. Although most of the traffic in the backcountry tends to be in the Williams Lake drainage, other areas of the forecast zone have a much shallower snowpack, especially near and below treeline. Although unlikely to trigger, that doesn't mean that you couldn't find an isolated slope in steep terrain where you could potentially trigger a very large persistent slab avalanche.
Faceted crusts and buried near surface facets that formed during the dry periods at the end of February and early March are the persistent weak layers that remain a concern.
Photo: Charlie Harrison (3/14/2024)