Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
Triggering a persistent slab avalanche is possible today at mid and upper elevations. The snowpack has overlapping weak layers of buried facets, crust/facet combinations, and buried surface hoar giving all aspects at least one problem layer. It has been a busy week with both natural and human triggered avalanches on all these layers. This recent avalanche activity re-enforces the need for caution and avoidance.
Avalanches have been especially active in the elevation band where recent warm temperatures have warmed previously dry snow, often at the upper end of the mid elevation band.
Some layers, like the buried surface hoar, have produced obvious red flags and widespread collapsing. Others, like the depth hoar at upper elevation, have shown no red flags before producing a large avalanche.
Take the time to dig and investigate the snowpack where you are looking to ski or ride. If you find a slab over weak, sugary snow, stick to slopes under 30 degrees. Surface hoar can be identified as a thin grey line across your snowpit wall. If you find it, be especially cautious. Buried surface hoar can create avalanches for weeks and is a common weak layer in fatality avalanches.
(1/20/2024)