Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
The snowpack is adjusting to last Friday's storm and it's slowly becoming more comfortable in its own skin. However, we need to remember, our Persistent Weak Layer, buried in the mid portion of the snowpack is in its teenage years and it doesn't take much effort to get it riled up. In fact, on my field day Sunday, I experienced sudden collapses of the snowpack along with muted whoomphing sounds... all indicators of a weak, rotten snowpack with a dense layer of snow on top. So, while the surface snow may feel good to go, we need to think about not only the snow we're riding in, but also the snow we're riding on. And remember- any slide triggered will break several feet deep, and a couple hundred feet wide, failing on one of the many persistent weak layers of faceted snow in the snowpack (see the photo below).
There are three things that make the setup deceptively tricky:
- There's not an abundance of in yer face clues like natural avalanches, but many steep slopes wait for a trigger like us to roll along and knock the legs out from underneath.
- You won't have to be on steep terrain in order to trigger a slide. Just being near or under a steep slope is enough to tip the balance. And previous tracks on the slope shouldn't be your barometer of slope stability. It could easily be the 3rd or 4th or 10th person that triggers an avalanche.
- Several wind events, including last night, created dense, cohesive slabs that may be hard to detect. Older slabs are now buried in our pack and are harder to trigger until you hit the right spot on a slope, which of course, we can't see. The resulting avalanche is a thick, hard slab that easily ruins your day or perhaps your season.
Image below clearly shows a junk show. If you wouldn't build your house on a foundation like this... don't bet your life on it.
Video describing how you can trigger avalanches from below.