Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 4
The biggest clue to avalanches is of course, avalanches! Problem is... you don't look around the range and see avalanches everywhere. In fact, so much of our recent natural avalanche activity was nearly erased with avalanche paths quickly refilling as the January 13th/14th storm raged. So now comes the tricky part... it takes a sharp eye to put together the pattern, size, and scope of our recent avalanche cycle and to get a handle on the characteristics and personality of our current avalanche dragon.
Remember- the persistent layer of weak, sugary snow formed during the mid December dry spell hasn't gone away. In fact, it's now buried several feet deep and a very strong piece of snow, a slab, rests on top. And while the snowpack isn't nearly as active as just a few days ago when it reached its boiling point, we have to remember, it's still simmering. Sure, all the right ingredients have to blend together to trigger a slide today, but just like Emeril in the kitchen, when it all comes together... Bam!... your goose is cooked and you'll be staring down the barrel of a very dangerous avalanche. (disclaimer... no geese were injured or cooked in the making of this metaphor :)
Triggering a slab avalanche on the now buried mid-December drought layer remains likely, especially if you collapse (whoomph) a slope near a thin area of snow (like around a buried rock, boulder, or bushes barely covered with a thin facade of snow).