Northwest Avalanche Center

Observation: Public

All Observations

Observation Details

Name:
Nate Hough-Snee, Evan Honeyfield, Andrew Breibart
Observation Date:
February 21, 2022
Submitted:
February 28, 2022
Zone or Region:
East Central
Activity:
Skiing/Snowboarding
Location:
Entiat/Copper

Observed Avalanches

Did you observe any avalanches? 
Yes
Avalanche Type:
Dry Loose (Sluff)
Size:
Size 2: Could bury, injure, or kill a person
Elevation:
6000'-9000'
Aspect:
N
Comments:
Noted dozens of recent dry loose avalanches in steep terrain from the 19-20 February storm above the Copper drainage and the Entiat headwaters. Avalanches seemed isolated to steep features and were largely L-N-R2-D2 running 200' to 1000'. Notably, none of these stepped down to deeper layers below the Valentine's crust, indicating the February high pressure had created a strong bed surface.

Signs of Unstable Snow

Did you see shooting cracks? 
No
Did you experience collapsing or whumpfing? 
Yes, Isolated

Observations

(Composite ob from several days 18-22 Feb) A day after the 19-20 Feb storm, at 5500' on north we noted CT results that failed on facets below the Valentine's crust (14 Feb) with 10-12 taps and resistant or sudden planar shears. In some cases, multiple crust-facet layers failed on the same tap. While these results on isolated columns were clean, the larger crust seemed to bridge under a skier's weight up until about 7000', where 14 Feb crust became thinner and the likelihood of a cornice, wind slab, or skier triggering slab avalanches became more likely. HST ranged from 6-10cm at 4000' to 40cm at 7000' where winds had created soft drifts and scoured some areas to crust from the February high pressure.

Another major note is that crevasses were out with large cracks below Fernow and Copper, even after the 19-20 Feb storm. By 22 February, the storm had settled out nicely and skiing had improved dramatically over the 14 Feb crust.

Media

5500' north near Copper Mountain. We found the 19-20 Feb storm over a dagwood sandwich of crusts and facets at 5500' from late January and early February storms. The upper layer was reactive a day after the storm on isolated wind slabs.
Mapping of crusts and facets at 5500' - compression tests failed on the top crust when isolated but this layer was not reactive when traveled over until 7000'.
That were abundant dry loose that ran on steep east facing terrain ATL
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