Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Poor snowpack structure exists on all slopes facing the north half of the compass. In these areas the entire snowpack is loose, weak, and faceted beneath the Christmas rain crust. Red flags such as collapsing and whumphing are not widespread but they are occurring. In spite of the poor structure, we've had surprisingly non-reactive test results. In my travels yesterday, however, I was able to produce a score of ECTP23 in an extended column test on a NE aspect right around tree line at 11,000'. On Sunday, Chris and Morgan Orozco produced a score of ECTP7 in an extended column test also on NE aspect. Read their complete observation here. These are clear indications that it is possible to trigger an avalanche on a buried persistent weak layer.
The likelihood of triggering an avalanche largely depends on the strength and thickness of the rain crust in various locations. If you are into splitting hairs, the most likely areas to find trouble are right around tree line, in places where the rain crust is very thin. Personally, I'm just not willing to trust the strength of the crust with my life and I'll be avoiding northerly aspects steeper than 30 degrees for awhile.
Results of my extended column test yesterday. Note the thickness of the slab failing on deeply buried facets near the ground. An avalanche of this size and depth would be very dangerous.