Observation: Mill Creek Canyon

Observation Date
1/5/2016
Observer Name
White, Staples, Staff
Region
Salt Lake » Mill Creek Canyon
Location Name or Route
Wilson, Alexander
Weather
Sky
Overcast
Precipitation
Light Snowfall
Wind Speed
Calm
Weather Comments
Warm and humid with low lying cloulds, a few sucker holes of sun intermintantly, periods of light snowfall, dead calm on the ridge line.
Snow Characteristics
New Snow Depth
1"
New Snow Density
Medium
Snow Surface Conditions
Powder
Dense Loose
Wind Crust
Melt-Freeze Crust
Damp
Snow Characteristics Comments

About 1 inch of new snow laying on a variety of surfaces, melt freeze crust on S facing aspects, wind crust in the higher wind exposed terrain, settled powder in sheltered terrain, and damp snow up to about 8200ft.

Comments

Hadn't spent much time in Millcreek since the Christmas avy cycle and wanted to get a handle on what avalanched. Travel was up the Bowman trail in Millcreek, Yellow Jacket, Toots to Boots into Alexander Basin, Depth Hoar Bowl, and the exit out Bonus Bowl into Wilson Fork. Toots to Boots had avalanched, most likely midway through the Christmas cycle, Mark performed a ECT in the skiers left side starting zone that had not slid, profile included. Depth Hoar Bowl had avalanched wall to wall, and a few of the lower roll overs also avalanched, also looked like most of the NW facing paths off the top of Wilson had avalanched into Alexander Basin, as well as most of Bonus Bowl. Probing the snow in Depth Hoar Bowl revealed that most of the facts in the basement had been destroyed, with only a thin veneer of snow left in the upper starting zone, and fairly stout debris in the bottom.

Photos: ECT in Toots, looking down Toots, in and out low lying clouds, and damp snow at about 8200ft

Staples comments:

Two pits around 9000 ft on ENE aspects. I think you can get a crack to propagate in the facets near the ground, but I think you will have a really hard time getting it started especially in places w/o a heavy wind load. Until the balance of stress vs strength is altered by new snow, triggering a deep slab will be difficult but not out of the question.

This first ECT had a very rough fracture surface. The fact that it propagated is more important, but the uneven fracture surface is perhaps a sign that things are moving in the right direction??? I'm not sure.

Video

The next pit had a much cleaner fracture surface because it broke on facets above an ice crust. What was interesting here is that just 5 feet to the south, the ECT would not propagate and snow depth was only 5 cm deeper. I think part of this is a result of irregular snow cover in November and early December. Either way an ECTP is a red flag, but getting more and more ECTN's is a sign that we're moving in the right direction (ie-these facets are getting stronger and healing). Also, these two different results are not random variation in the tests. The snowpack felt very different as I was shoveling from one place to the other - that's why I dug and extra wide snowpit

Thinking low in most terrain, maybe stick with moderate in upper elevation, steep rocky, wind loaded terrain.

Today's Observed Danger Rating
Moderate
Tomorrows Estimated Danger Rating
Moderate