Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Ted's snow profile from the North Slope reveals the big Thanksgiving storm resting on weak snow near the ground.
Here's the problem-
As the snowpack settles it's gaining strength... and that's good news. The bad, not so in your face, you need to do a little homework news is... upper elevation slopes facing the north half of the compass harbor old October snow (weak layers). While not as widespread as earlier this week, upper elevation slopes facing the north half of the compass continue producing big, booming collapses (whoomphing sounds) and shooting cracks. This is a huge red flag indicative of dangerous avalanche conditions. As a matter of fact, all you need to do is a little investigating. Take your shovel out, dig down a few feet and you'll clearly see the overall snow structure suggests we've got a sketchy snowpack. This is the type of setup where we don't even have to be on the slope in order to trigger a slide, we just need to be connected to it. What this means is... we can initiate avalanches from a distance or even low on the slope. Once triggered, even a small avalanche may break a bit deeper and wider than you might expect, failing near the ground, revealing obstacles hidden under the thin facade of our early season snowpack. Remember- any slide could easily result in a season ending injury if you get raked over stumps, rocks, or deadfall.
It doesn't mean we can't ride, but what I do know is the best way to avoid unpredictable avalanche conditions is to avoid where it exists. We can still have a great day by playing in big open meadows and simply staying off of and out from under steep, upper elevation terrain facing the north half of the compass.