Observation Date
12/31/2021
Observer Name
Mark Staples
Region
Uintas » Shingle Mill
Location Name or Route
Mud Flats area
Comments
I was surprised how easily the ECT broke and propagated. It was on my last tap swinging my arm from the elbow (ECTP20), but I thought that I was going to have to give it hard taps swinging my arm from my shoulder becuase the weak layer has such a thick slab on top of it.
However, this thick, supportable slab made it a little harder to have widespread collapsing. We heard several collapses, including a very loud, tree shaking collapse.
Let me make a key point - triggering a collapse IS EXACTLY THE SAME AS TRIGGERING AN AVALANCHE. The only difference is that the slope is not steep enough to slide, so you don't get an avalanche. However, all the other processes in an avalanche occur in a collapse.

Video below shows how deep the new snow is. Unbelievable.
Video
Comment about the danger rating -
There are several ways to think about avalanche danger. View the danger scale below. Notice the columns labled "travel advice", "likelihood of avalanches", and "avalanche size and distribution".
The travel advice for HIGH danger fits our current situation on northerly facing slopes (as well as W, E, and SE) very well - "Very dangerous avalanche conditions. Travel in avalanche terrain NOT recommended."

Today's Observed Danger Rating
High
Tomorrows Estimated Danger Rating
High
Coordinates