Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 4
Strong snow on weaker snow, this is what the structure looks like at the crown of the sled triggered Double Hill avalanche from earlier this week.
And this is what it looks like in a snowpit. Mark and Micheal J stomped around the Hoyt Peak environs Wednesday confirming all our snowpack suspicions... the weak, sugary, and persistent weak layer (PWL) in the mid portion of our snowpack is still quite reactive.
The good, the bad, and the potentially ugly-
Our recent round of ultra-blower pow isn't going to wake up the avalanche dragon, but pull back the curtain and a more nefarious setup is revealed... and here's what's going on. Last weekends wind formed a dense, strong slab, but that solid layer rests on weaker snow (Persistent Weak Layer or PWL) formed during the mid November dry-spell. Now here's where it gets tricky, this setupgives us a false sense of snow stability, because it feels bomber and good to go underneath our skis, board, or sled. In fact, this combo often lures us well out onto steep slopes before weak layers fail, allowing avalanches to break well above us and the whole roof crashes down. So yes, I'm thinking not only about the snow I'm riding in, but also the snow I'm riding on. Here's where the rubber hits the road and what makes things tricky right now... any avalanche that fails near the midpack weakness (PWL), is gonna break deep and wide and it's gonna be dangerous.
Unless you take your shovel out, dig down and investigate a bit, you can easily get lulled into a false sense of snow stability because the snowpack has gained a substantial amount of buoyancy. Yep, that pack's got a whole lotta body... baby :)