Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Poor snowpack structure exists with consolidated slabs resting on buried persistent weak layers of loose, sugary, faceted snow on many aspects. However, the snow is getting stronger with time and relatively warm temperatures within the lower snowpack. Extended column tests were not able to produce failures that propagated across the column (ECTN28 x2). Two propagation saw tests did, however, suggest that the "propensity for propagation" is still present (PST30/100 (End) @ 32 cm and 15 cm). The most dangerous areas are on slopes above treeline that face NW-N-SE where wind drifted snow has created slabs 1'-3' deep on top of these buried weak layers. Once triggered, these slab avalanches would be large and destructive.
The image below shows the relative hardness of each layer, sort of like rock layers in the Grand Canyon. Picture building blocks stacked on top of one another with varying strengths and thicknesses, and note the very precarious situation between 10-20 cm. This is the layer of weak, sugary snow that the rest of the snowpack is sitting on.
I did notice some weak snow (near surface facets) near the top of the snowpack yesterday. While not a problem now, these small, sugary grains could be an issue once they are buried.