Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A persistent weak layer of faceted snow that developed during the cold dry period in mid November exists on aspects that face W-N-SE. Incremental loading from recent and wind drifrted snow has kept the pressure on this weak layer but the danger is slowly decreasing. The greatest danger exists on slopes facing NW-N-E, where wind drifted snow has built thick slabs on top. These hard slabs are 1-4' thick and can produce very large, deep, and potentially deadly avalanches. Slopes steeper than 30 degrees should be avoided in these areas.
I dug a snowpit and peformed an extended column test on a NE aspect at 11,200' yesterday and acheived propagation on 18 taps. In the photo below you can see how a well defined slab failed on the persistent weak layer of facets in the middle of the snowpack.
This chart illustrates the layering in the above photo. We are looking for harder layers over weak layers. In the chart, the further a layer is drawn to the left, the harder it is. From the chart, you can see the weak layer where failure occurred between 40-45 cms.