Northwest Avalanche Center

Observation: Public

All Observations

Observation Details

Name:
Enji Cooper
Observation Date:
March 27, 2021
Submitted:
March 29, 2021
Zone or Region:
East Central
Activity:
XC Skiing/Snowshoeing
Location:
Tronsen Ridge/Meadows

Observed Avalanches

Did you observe any avalanches? 
Yes
Avalanche Type:
Wet Loose
Size:
Size 2: Could bury, injure, or kill a person
Elevation:
Above Treeline
Aspect:
N
Comments:
Observed a variety of wet loose avalanche debris, ranging from D1 (along the ridge) to D2 (Diamond Head), around the Tronsen Ridge basin on northern aspects. One instance we were able to look at seemed to be trigger by an increase in temperatures on an NE facing aspect of the ridge and was part of a cornice.

Also triggered a lot of wet loose debris (melon-sized pinwheels mostly, but some fist-sized rollerballs) that ran for 50' or so in our down track route.

Signs of Unstable Snow

None reported

Observations

Started off early from 47.3378, -120.5664. Proceeded along NF-7420 and pushed N up lower angled ridge to Point 5367. Much of the ascent was snow free up until Point 5367 along W facing slopes (we stuck to game trails and more durable surfaces wherever possible). Point 5367 had some ice and low coverage snowpack.

The saddle between Point 5367 and Tronsen Ridge "Peak" (Point 5575) (47.3392, -120.5366) was snowier, but didn't exhibit any major instability concerns.

The saddle/ridge spine up from Point 5575 to Point 5940 (47.3341, -120.5304) was where we started exercising caution due to large cornice overhangs and visible/anecdotal instabilities between the top-layer of wind fetch (approximately 3"~6" deep) and the lower, more consolidated/icy layer.

At higher elevations between Point 5940 and Tronsen Head, we encountered variable snow coverage: some areas were bare/exposed rock -- other areas were deeper fetch in the saddle/under the trees (where it was more shaded). Down lower, the snow was more consolidated/firm earlier on in the day.

Getting up the ridge from the saddle to Tronsen Head was more difficult due to non-consolidated dry-ish powder (wind fetch/storm snow), but I didn't observe the slab breaks I had seen near Point 5940.

Getting down from Tronsen Head to Tronsen Meadows involved a down track starting near 47.3126, -120.5452, heading approximately due N (this area was chosen due to slope angle/higher tree cover). We accidentally went a bit too far skier's left in areas running into slope angles greater than 35°, which forced us to course correct (skier's right) to lower angled slopes (much of what was observed here was D1/R1 wet loose debris). Once we got down to approximately 5200', the risk was reduced due to lower slope angle and less wind fetch.

Media

Starting the march towards Point 5940.
Cornices up Point 5940 (1/2).
Cornices up Point 5940 (2/2).
Cornices near Tronsen Head.
Windy Knob and Diamond Head from Tronsen Ridge

Advanced Observations

Observed Avalanche Problem #1: 
Cornice
Comments: 
Lots of large cornices along N aspects of the ridge. My snowshoeing partner and I were ducking and dodging multiple cornices that were at least 1' high between Point 5575 and the next high point (Point 5940) (47.3341, -120.5304) due SE of Point 5575.

After that it was mostly smooth sailing along the ridge, but we observed very large cornice overhangs from Point 5940 over at Tronsen Head, Windy Knob, and Diamond Head.

Getting over to Tronsen Head, we observed (in greater detail) the cornice overhangs at Tronsen Head, Windy Knob, and Diamond Head.
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