Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 4
Ted was near Gold Hill yesterday and finds the very apparent mid November faceted snow layer, buried in the mid portion of our snowpack. More on Ted's travels HERE.
The sugary, weak faceted snow buried in the mid portion of our snowpack was just getting comfortable in its own skin, adjusting to last weeks big storm, and the lack of recent avalanche activity suggested a slow turn towards stability... good news. But today's big wind, coupled with forecasted additional water weight and storm snow is gonna reactivate our mid pack weak layers and bring 'em back to life. Problem is... strong snow rests on weaker snow, giving us a false sense of snow stability, luring us well out onto steep slopes before they break 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 our problem child, the persistent weak layer or (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 and will feel strong and solid underneath or skis, board, or sled.
Obvious signs of unstable snow include cracking, collapsing, and whoomping noises as well as natures freebie... natural avalanches!
We taught a Sled 101 class yesterday in the Currant Creek zone and found similar structure on the south half of the range.