Observation: Mill A

Observation Date
3/8/2015
Observer Name
Bruce Tremper
Region
Salt Lake » Big Cottonwood Canyon » Mill A
Location Name or Route
Mill A Basin
Weather
Sky
Clear
Wind Speed
Light
Weather Comments
Another bluebird, not a cloud in the sky, pleasant temperatures, slightly cooler than yesterday with the high near 40. Life is good.
Snow Characteristics
New Snow Density
Medium
Snow Surface Conditions
Dense Loose
Faceted Loose
Melt-Freeze Crust
Damp
Snow Characteristics Comments

It's the usual mixed bag of snow surface conditions you would expect 5 days after the last storm. Nice, dry, dense, settled powder and near surface faceted snow on the slopes that face the north quadrant and various kinds of sun crusts and damp to wet snow on all the other aspects.

Red Flags
Red Flags Comments
Not many red flags anymore because things are settling out nicely. You can still probably get some wet, loose avalanches on the steep, sun exposed slopes if you try. You might be able to pop out a dry slab on north through east but for the most part things are fairly well settled.
Avalanche Problem #1
Problem
New Snow
Problem #1 Comments

I dug 2-3 snow profiles yesterday on Little Water Peak and another profile and a fracture line profile today in Mill A Basin on the north through east facing slopes. Profiles were very consistent in all areas. I did over a dozen compression tests which all required pretty good force to get things to collapse on near surface faceted snow or recrystallized graupel buried about 1.5 feet deep in the snowpack. You get a fairly clean shear but probably Q2, popping out without much energy. It usually takes the first couple shoulder taps to get them to go. I did probably 8 Extended Column Tests yesterday and today and could not get any of them to propagate. They just mushed down under the shovel, then when I moved the shovel over to the middle of the column, it would pop out the rest of the column. So not real impressive results. It behaves like you would expect snow to behave 5 days after the storm when the weak layer is adjusting to its load. Lots of people are skiing steep slopes next to old avalanches from 5 days ago and getting away with it. (A little too bold for me, though.)

Avalanche Problem #2
Problem
Wet Snow
Problem #2 Comments

Not much fresh, sluffs or slabs today and most of the activity occurred yesterday or the day before. The snow seems like it's been there done that. I noticed a fair number of drainage channels (rill marks) on the south facing slopes, which mean that drainage channels have formed within the new snow and it's a sign of stability. I'll bet you could still get some wet snow going in steep terrain in the heat of the day of you pushed on it. But for the most part, it has significantly slowed down.

Comments

Nice view across to the larger peaks in Broads and Mill B South. You can see lots of slab activity during the storm 5 days ago. See the zoomed-in photo below in Broad's Fork

It's hard to tell from the low resolution photos allowed on our website, but when I zoom into the full rez photo I can see a number of slabs in the upper bowl of Broads, in the headwall and along the Mill B South ridgeline. Perhaps 40% of that terrain slid during the storm as natural avalanches.

The east aspect of Raymond Peak. that drains into Mill A Basin This is like a quiz in an avalanche class. How many things can you see going on in the snow? First, there's the little drama in the foreground with the coyote track and mouse track. Then, in the background, you can see dry slabs and sluffs that came down during the storm 5 days ago. Over the top of them, you can see the more recent wet activity, probably from yesterday, and you can also see some ski tracks.

Another avalanche class quiz: The vertical channels are called "rill marks" or "drainage channels." They form within new snow after melt water has percolated through it to form drainage channels under the new snow. They are actually a sign of stability since they indicate that the plumbing has been established.

A nice specimen of a snow snail or pinwheel. These are gravity's snowmen and they roll down the slope as new snow rapidly gets damp or wet from strong warming.

In the upper Mill A Basin headwall, you can see the east facing slope on the right is producing some wet sluffs while the north facing spur ridge on the left has a slab from the last storm, probably 5 days old. Dry snow on the shady slopes and wet snow on the sunny slope.

Zoomed into the avalanche, which is 1 to1.5 feet deep and perhaps a total of 200 feet wide. I did a fracture line profile on the looker's left flank. It slid on near-surface faceted snow that was on the surface before the storm on Tuesday. My test showed that things have settled down quite a bit as it took quite a bit of force to get the compression tests to fail and the extended column tests did not propagate. Translation: that's a good thing.

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