Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 4
The biggest clue to avalanches is.... avalanches! Occurring during the mid December storm, sure it's old news, but the slide in the image above, to the southeast of Tower Montain, clearly illustrates the type of avalanche we're dealing when we talk about a persistent weak layer.
But wait.... there's more!
First, the good news-
Our snowpack is slowly healing and both snow structure and lack of avalanche activity reveals why it's been a over week since we've seen or heard of any avalanches failing on weak, old snow layers near the ground.
But second and most importantly...
There's a persistent weak layer near the ground, and once initiated, avalanches have a distinct possibility of breaking deeper and wider than you might expect.
Personally, I don't entirely trust anything in the snowpack I can't manage, so I'm going to continue avoiding terrain that harbors questionable snowpack structure. Of course the usual suspects come to mind... steep, rocky, upper elevation slopes facing the north half of the compass is bulls-eye terrain and should be considered suspect. With all the great coverage across the range and so many other riding options, there's no reason to roll the dice or pull on the dogs tail.