Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
The storm early last week added more load to our well-established persistent weak layer that is now buried around 1-2 feet deep in this zone. The highest concentration of avalanches occurred in the western portion of this zone (see observation from the Soldiers) where more snow fell, but natural slides were also observed in the Wood River Valley and in Bassett Gulch on the backside of Baldy.
In the mountains near the Wood River Valley, the greatest likelihood of triggering an avalanche exists on wind-affected slopes where a thicker slab overlies the fragile weak layer. In the western portion of this zone—including the Soldiers and Dollarhide areas—the instability is widespread, and even wind-sheltered slopes remain dangerous.
There are two key factors that point to this instability being especially long-lasting and unpredictable: 1) the buried weak layer is especially bad, and 2) this weak layer has been very slowly loaded over the past three weeks. As time goes by and the obvious signs of instability diminish, it requires more and more discipline to choose appropriate terrain—read more on that in the Forecast Discussion below. We urge backcountry skiers and riders to continue to choose low angle slopes and to pay extra attention to the terrain they're "connected" to. Remotely triggering an avalanche from below, above, and to the sides of steep slopes remains a very real possibility.