Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Most of the avalanches from the last cycle (March 14th) stepped-down to a layer of weak, faceted snow near the ground, and human triggered avalanches remain possible on similar slopes that have not avalanched. New snow and wind have increased the chances of avalanches today. The greatest concern is on wind loaded slopes that face NW-N-E-SE near and above treeline. Yesterday on a NE aspect near treeline, I found large (2-3mm) angular depth hoar still present at the bottom of the snowpack. 3-5 feet of dense snow is resting on top of these weak layers, and although it is difficult to trigger an avalanche failing on these weak layers, if you find the wrong spot, the possibility still exists to trigger a large and destructive avalanche. I did a couple of extended column tests, which did not produce any results, however, as you can see in a propagation saw test below, we still have a deep, persistent slab problem. Suspect areas and likely trigger points include: thin snowpack areas consisting of steep, rocky terrain, thinner snowpack areas along slope margins, and near rock outcroppings or trees. Today, reduce your exposure by keeping your slope angles below 30 degrees.
The following video (3/17) of a propagation saw test on a NE aspect at 11,200' illustrates the kind of avalanche problem we are dealing with.