Incident

Avalanche: Six Mile Canyon

Travis Otten, Brett KobernikSkyline
View on map

Quick report

Slope Angle
34°

Avalanche

Slab Width
46 m
Weak Layer
Facets
Trigger Type
Snowmobiler
Vertical Fall
213 m
Avalanche Type
Soft Slab
Slab Thickness
152 cm
Trigger Detail
Repeater
Start Zone Aspect
East
Avalanche Problem
Persistent Weak Layer
Start Zone Elevation
3292 m

Snowmobiler triggered this slide near the fracture line and was caught and carried but was able to regain enough control of his sled to maneuver out of the slide before it stopped. It broke deep into older weak snow.

We attempted to visit the site on Saturday but heavy snowfall, poor visibility and additional avalanche concerns hampered our goal. We did obtain some good info though. This was a very curious avalanche.

The slide was triggered Friday. That day, Travis climbed up the bed surface to the fracture line. He reports it was chest high, about 5' deep. The slide broke to the ground. It contained about 4 feet of strong snow with around a foot of facets at the ground.

Near the debris pile, we probed and found a total of 7 to 8 feet of snow. The snowpack structure was much different (image below) than what Travis found at the fracture line. It was much deeper and much stronger near the debris pile. This doesn't make sense because, given the leeward facing wind loaded slope, the snowpack should've been deeper at the fracture line than in the flats down below. This leads me to believe that the avalanche path already released earlier this season, leaving a shallower snowpack and thus, a weaker snowpack. This has been a theme in regions to our north this winter but this is the first case that I believe this to be true here on the Skyline.

Incident

Number Caught
1
Number Carried
1