Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 4
We are trending in the right direction and recent snowpack stability tests suggest we are turning the corner.
So here's what I know... in most terrain the snowpack is becoming thick and strong, and deep dangerous avalanches are becoming harder to trigger.
I also know that all I need to do is find a shallow, weak portion of the snowpack, perhaps around a rock or bush that I can't see underneath the snow, collapse the slope (whoomph), and now I'm staring down the barrel of a dangerous avalanche. In addition, I know first hand from crawling around recent big avalanches that the common theme is they've occurred on steep, rocky, upper elevation, wind drifted slopes facing the north half of the compass, along with slopes that avalanched earlier this season and have a shallow snowpack.
What I don't know... where exactly these weak points exist in the snowpack and whether or not I can trigger something that breaks to the ground.
In this business, one of the keys to longevity is embracing the concept of avoiding bulls-eye terrain where unmanageable avalanche dragons live. So if there's uncertainty in the snowpack... I simply avoid the unknowns.
So for today, I know I can still have a great day of riding safely by managing my terrain choices and steering away from steep, rocky slopes.
It all looks white and even until we see what's underneath the snow we're riding on-
The last avalanche noted breaking to weak snow near the ground was about a week ago. While getting harder to initiate, the natural slide in the image above was most likely triggered by cornice fall and fits the notion of avalanches breaking to the ground once a trigger finds a weak, shallow portion of snowpack, generally in steep, rocky terrain.
Here's what our weak snow near the ground looks like and Cody's take... "4-6 mm Depth Hoar crystals found in our deep snowpit in the Humpy Creek drainage. Hard to trust a depth hoar snowpack even when buried this deep..."