Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Today, human-triggered slab avalanches failing on a buried persistent weak layer could be large and life-threatening. During the last storm, heavy snowfall and drifting by winds from the west overloaded slopes plagued by widespread buried layers of weak, sugary snow or facets and feathery surface hoar that developed during the prolonged December dry spell.
- Avalanches could be triggered remotely, from a distance, or worse, from below.
- Collapsing or whumpfs and shooting cracks indicate unstable snow.
- Avalanches are possible even when there are no obvious signs of instability.
- Exposed slopes, where the wind drifted the heavy new snow, developed dangerous wind slabs that now are overloading buried persistent weak layers. Watch for and avoid stiffer drifted snow on the lee side of prominent ridges and in and around terrain features like sub-ridges, gully walls, mid-slope rollovers, and cliff bands.
- ALSO - with unseasonably warm temperatures and rain, the low elevation snowpack is now saturated. Coupled with sitting on top of weak snow, it is possible to trigger an avalanche in unsuspecting terrain where the snow is deeper like the steep banks next to the Logan river.