Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
I would expect to see dry loose avalanches on a density change within the new snow. Shovel tilt tests are a great tool for finding weaknesses within the storm snow.
There are tricky avalanche conditions out there right now. The old/new snow interface from February 21 is still producing propagation with extended column tests and I will be digging down at least 3' to the old/new snow interface from last week's storm to see how this layer is reacting before traveling on terrain over 30 degrees. My snow pit from Upper Big Cottonwood Canyon showed this layer buried 2' under the snow surface.
It is a good time to back off and seek soft turns on slopes less than 30 degrees until these interfaces show us they are no longer capable of avalanching.