It sounds like the wind started to transport the light surface snow into wind slabs in the alpine and at treeline. There isĀ about 140 cms below treeline in the Duffey Lake area, with 30 cms ski penetration and waist deep foot penetration at treeline. At 1900 metres on a NE aspect there was 60 cms of very light (Fist) density snow above slightly stiffer (4 Finger) snow. Snow stability tests showed only mid storm collapses. The Coquihalla also has a well settled "right side up" snowpack that is about 190 cms deep at 1550 metres elevation. "Right side up" means that the surface layers are light and soft, and then the layers get progressively more dense as you move down through the snowpack. The ski penetration has been reported to be about 40 cms and the foot penetration is very deep at 80 cms. The light snow is causing a lot of sluffing in steeper terrain, but is not reacting as a slab. The November crust has not been found in the Coquihalla, although we don't have any reports from the high alpine. Conditions may be quite different in the North of this region, please email us your observations if you are out in the field.
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