Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
The pre-Thanksgiving storm created all the ingredients necessary for avalanches. Natural activity has ceased because the snowpack has adjusted to the load. However, the weight of a skier or rider can still trigger an avalanche because of the poor snowpack structure that exists on slopes that face W-N-E-SE. Snow-savvy backcountry travelers, myself included, continue to avoid any steep slope that harbors the dangerous strong-over-weak setup.
This avalanche from the Wasatch is a great example of the instability we are currently dealing with. What stands out is that “most of this slope had a couple dozen ski tracks on it.” When persistent weak layers are involved, tracks on a slope do not indicate stability.
The photo below shows the current setup, with strong snow (the slab) on top of the weak layer.