Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
The most likely places to trigger an avalanche are on slopes facing the north half of the compass, particularly east facing slopes, loaded by recent winds. In terrain with these characteristics, avalanches may break 1-2 feet deep, failing on a persistent weak layer of facets generally found about a foot above the ground.
Common characteristics (1) The snowpack is generally weak, rotten, and full of facets. Even the snow surface has faceted which made for acceptable skiing conditions. (2) Strong, west and northwest winds blew last week, forming hit-or-miss wind slabs on top of this weak, sugary mess.
What does all of this mean? Below treeline, the snowpack is basically one big persistent weak layer lacking a slab on top to create an avalanche. Near treeline snow depths increase some, and there is more of a slab on top of the weak snow, but they aren't nearly as sensitive as they were last week.
Photo - north aspect near 10k feet. Snow layers near the shovel blade is snow that fell in November and early December. The weakest snow is the obvious stripe of facets near the top edge of the shovel blade. That stripe of weak snow sits on a decomposing crust. Snow near the shovel handle is the slab that can create an avalanche. Slopes with the added weight of wind drifted snow on top of this layering are the ones most likely to avalanche.
Ted was out Friday and says.... "It felt like the theme of the day was cracking and collapsing of the weak snowpack and some of the collapses were quite attention getting. I was not anticipating too many red flags today, but the Gold Hill zone felt fairly unstable and a little on the "spooky" moderate side of the danger scale." Some sage advice from a super knowledgeable avy, savvy pro who knows the Uinta's better than all of us.... combined!