We are trending in the right direction and recent snowpack stability tests along with the lack of avalanches failing on weak snow near the ground suggest we're turning the corner. Also streaming in from the good news department is this... most terrain where the snowpack is becoming thick and strong, deep dangerous avalanches are becoming harder to trigger. All encouraging news for sure, but we've got to remember there's a lot of terrain that makes up the landscape of the western Uinta range and I'm not entirely convinced all slopes are good to go. However, our theories will get tested as the next series of storms should add a substantial amount of snow and water and help us determine the strength of our deeply buried weak layers. In the meantime, let's reflect on how persistent weak layers work and remember that all I need to do is find a shallow, weak portion of the snowpack, perhaps around a rock or bush that I can't see underneath the snow, collapse the slope (whoomph), and now I'm staring down the barrel of a dangerous avalanche. What I don't know... where exactly these weak points exist in the snowpack, but steep rocky slopes are certainly high on the suspect terrain list and should be avoided today.