Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 4
Heavy snowfall and strong winds have overloaded a persistent weak layer (PWL) of faceted snow down near the ground on mid and upper elevation aspects facing west through north and east. This weak layer formed from snow that fell earlier this Autumn, and once we buried this weak layer beginning on December 9, the PWL has become reactive with avalanching on every loading event of new snow and/or wind.
We have once again rapidly overloaded this weak layer with heavy snowfall and strong west/southwest winds, creating very dangerous avalanche conditions. On my field day yesterday in mid-elevations along the Big Cottonwood and Millcreek ridgelines, I was finding this weak layer to be very reactive to stability tests.
Avalanches failing on this weak layer may be triggered remotely (from a distance) or from below. Any avalanche failing on this PWL may break down 2-6' deep (possibly deeper) and propagate hundreds of feet wide.
Do not travel on or below slopes approaching 30 degrees or steeper on mid and upper elevation aspects facing northwest through east.
The photo below shows the poor structure of strong snow over weak snow.