HS-48"
Of note: Two areas of basal facets separated by a decomposing melt-freeze crust. The lower part of the mid-pack has consolidated to 2-finger hardness. Still very easy to isolate columns to the ground with a ski pole.
ECTP 21, Q2.5 at 40" below the surface (Yikes!) in the facets above the melt-freeze crust. This is spooky for several reasons including:
It is greater than 3' down, which is where it is supposed to be hard for a skier to trigger something from the surface. I typically feel 3' is not enough of a cushion.
It is late February, basal facets are typically healed way before now. I am not confident that they will heal at all this year.
Photos below:
1. ECTP 21 Q2.5 results, glove sitting on failure plane, facets on top of crust.
2. facets, rounding a bit but still very loose and weak.
Other photos:
1. Wind affect
2. Trenching thru wind drifts.
Overall a solid Considerable hazard above 8,000' on north aspects. I felt like I was tip-toeing around all day.
If anyone wants to get in touch with me about snow/avalanche questions in SW Utah, I can be reached at [email protected]. I would be happy to walk anyone through the observation process. All observations are appreciated.