Schooled in the Kindergarten couloir!

Quick report

Craig McGee · Jan 8, 2024 · Lake Louise

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Observation photo 1

Quick report

Weather
cloudy
Ride Type
steepSlopes
Riding Quality
good
Snow Conditions
hard, powder
Avalanche Conditions
avalancheConditionSlab

Weather

Max Temp
-35
Min Temp
-20
Wind Speed
windSpeedLight
Blowing Snow
light
Sky Condition
scatteredClouds
Wind Direction
SW
New Snow24 Hours
5
Temperature Trend
rising
Precipitation Type
none

Wind was picking up

Snowpack

Obs Type
point
Site Aspect
N
Site Elevation
2400
Ski Penetration
0
Test Failure Layer Crystal Types
facets

Avalanche

Run Length
1
Slab Width
1
Trigger Type
skier
Wind Exposure
downFlow
Avalanche Size
1.5
Trigger Sub Type
accidental
Start Zone Aspect
N
Start Zone Incline
20
Avalanche Character
persistentSlab
Crust Near Weak Layer
1
Number Of Avalanches
1
Start Zone Elevation
2400
Runout Zone Elevation
2275
Avalanche Observation
12hrsAgo
Weak Layer Crystal Type
facets
Start Zone Elevation Band
alp
Avalanche Occurrence Datetime
2024-01-09T03:31:00.000Z

40-50cm deep and 15-20m wide, steep convex feature. Believe it was a soft slab on facets over the December crust.

Incident

Group Size
3
Group Activity
skiing
Number Involved
1
Number Caught Only
1
Snow Depth Trigger Point
deep
Terrain Shape Trigger Point
convex

Decided to check out the Kindergarten couloir, as many people had been referencing that it had seen quite a bit of skier traffic and had a lot of avalanche debris in it. Usually, with this type of snowpack and early-season conditions, I would have kept it pretty simple, but my FOMO (fear of missing out) got the better of me. Upon arrival, the presence of significant sloughing and avalanche debris alleviated much of the uncertainty surrounding avalanches. Instead, the main concern became cornices (much, much smaller than usual) and sloughing from the sidewalls. On the way up, travel was on soft avalanche debris, which made the travel pretty arduous. I consciously avoided sidewall pockets untouched by sloughing, and opted to turn back approximately 100m from the summit as the avalanche debris diminished. The increasing wind and the perceived risk associated with relatively small cornices reinforced the decision. Regrettably, during the descent, I succumbed to the temptation of making turns on one of the sidewall ribs I had bypassed on the ascent due to a lack of traffic or debris effect. This relatively small pocket popped, creating an avalanche roughly 40-50cm? deep and 15-20m wide? (approximations, as I didn't crawl back up to investigate!), resulting in a 125m (vertical) ride. The distinctive "BANG" upon the slab release led me to believe it was a soft slab on facets over the December crust. This event was a good reminder (Kindergarten schooling!!) that even though we all desire to "get after it" and try to convince ourselves that we can "outthink" an early-season Rockies snowpack, it's still an early-season Rockies snowpack that should be respected and treated with a conservative mindset. Also, the terrain associated with this avalanche definitely reminds me of many sidewalls and pockets on many of the ice climbs in the Rockies.