Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 3
Although it feels like spring, the snowpack represents and looks similar to what we usually see in mid-winter. Over the past week we have seen persistent slab avalanches failing naturally, and triggered by humans 1-3' deep and up to a football field wide. Digging down with your shovel or track it is easy to see what is going on. The Uinta's have a snow structure that's complicated and harbors multiple layers of sugary, faceted snow. In the attempt to keep it simple, I turn my attention to the two types of terrain where the chances of triggering an avalanche are more likely, and I try to break them down below:
- Shallower areas of the snowpack, or that have avalanche repeatedly this season (areas with less than 150cm of snow)
- Steep, thin and rocky areas where I am more likely to find a trigger point.
Slopes that have similar characteristics to the ones above, are the exact slopes where we've seen recent avalanche activity. As Craig always says, when snowpack is the question terrain is our answer. With that in mind, I am still avoiding slopes with this avalanche problem and practicing patience as every slope will have its day, but some times we just have to wait to play.
This avalanche failed in a shallower area of the snowpack, around 120cm, that had most likely avalanched previously this season and is a repeater, learn more here - Thanks Chad and Michael for the obs and eyes on things!