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Observation: Sundance backcountry

Observation Date
12/28/2018
Observer Name
Staples and Covington
Region
Provo » Provo Canyon » North Fork Provo R. » Sundance backcountry
Location Name or Route
Timpanogos near Provo Canyon
Weather
Weather Comments
Clear and cold. Did not appear to have the same winds as the central and northern Wasatch.
Snow Characteristics
New Snow Depth
4"
New Snow Density
Low
Snow Surface Conditions
Powder
Snow Characteristics Comments
Very very low density powder. 5 star conditions.
Avalanche Problem #1
Problem
New Snow
Trend
Decreasing Danger
Problem #1 Comments
The new snow was poorly bonded and would produce dry loose slides or sluffs.
Avalanche Problem #2
Problem
Persistent Weak Layer
Problem #2 Comments
Facets at the ground exist. Will they create an avalanche problem?
  1. They need a rapid, heavy load to become a widespread problem. 2 inches of water weight (about 20-40 inches of snow depending on temps) in 12 hours would probably do it. Big storms from the southwest can certainly provide that kind of snowfall in these mountains.
  2. Cumulative loading (ie - small continuous loading events) could start to make them unstable. We felt they could hold a decent load, but we would be hesistant to jump into avalanche terrain where this layer exists until it had a chance to "adjust" to recent loading.
  3. Bad luck. The higher you go and the closer you go to N or NE facing slopes, your odds of triggering a slide on this layer go up. A heavy load of wind drifted snow could provide enough of a load to get a pocket to break 3-4 feet deep on this layer.
The last reason (luck) is why many avalanche pros and experienced backcountry travelers are waiting for (1) this layer to get buried deeper, (2) this layer to have more time insulated by the snowpack to gain strength, and (3) this layer to be tested by the weight of a large storm with no avalanche activity on it. Luck is not a good risk management strategy. After time, it could be "game on" to ride big north facing slopes. Patience is key. The snowpack is shaping up for that green light to come on in the foreseeable future.
Notice the temperature profile in the snowpit. The steep temperature gradient is confined to the upper foot of snow. Deeper layers have a low temperature gradient that is good for bonding of snow crystals. Facets take a long time to bond and gain strength, but being insulated by a thick blanket of snow promotes this slow healing process.
Where does this layer exist?
South aspects do not have this layer. North and Northeast aspects above 9000 feet have this layer. We dug at almost 9200 feet. Chris found this layer yesterday south of Provo Canyon. It was thicker and more obvious because he was a little higher (9500 ft) and the mtns south of Provo Canyon had received more early season snow than Mt Timpanogos.
Snow Profile
Aspect
Northeast
Elevation
9,200'
Slope Angle
34°
Comments
One red flag was the compression test that fractured with a good pop at 22 cm above the ground on 13 taps. It surprised us! The ECT did not break on this layer after 30 taps until we slammed the shovel with a drop kick. I'm not sure what the reason was for this discrepancy. My guess is that it was because the faceted layer was not continuous in this location. It was uneven across the width of the ECT column. It was much more consistent across the more narrow CT column.
We did not travel on slopes affected by the wind and the danger was low. At higher elevations or on slopes affected by wind, the danger would have maybe been moderate.
Today's Observed Danger Rating
Low
Tomorrows Estimated Danger Rating
Low