Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Although we received no reports of avalanches, the three human-triggered avalanches from Thursday in the Salt Lake mountains all ran on the same persistent weak layer (PWL) of weak, faceted snow that is found at the base of our 1-2.5' deep snowpack on mid and upper elevation slopes facing northwest through east. As this weak layer slowly adjusts to the weight of the storm snow from Tuesday, you may get fewer clues - such as cracking and collapsing - about this instability and tracks on a slope may give you a false sense of stability.
If you choose to venture onto slopes where this PWL exists, you will have to first dig down and look for the structure of strong (harder/firmer) snow on top of weak (softer/looser) snow (see image below). If you see this structure, it is possible you will trigger an avalanche up to 2' deep and over 100' wide.
On Wednesday, Drew was in the Powder Mountain backcountry where his pit results demonstrated this poor structure of strong snow on top of weak snow.