Total snowpack depths generally range from 60cm at treeline to 150cm in some alpine areas, while most areas below treeline are below threshold depths for avalanches. The main snowpack feature is a rain crust buried early November and now down around 80cm at treeline. A weak layer of facets sitting on top of this curst recently gave very easy sudden collapse compression test results as well as moderate extended column test results that propagated across the entire column, in the Whistler area. Widespread whumpfing and cracking on this layer has also been reported. Because this weakness is so close to the ground in most areas, associated avalanche activity will likely be limited to slopes with smooth ground cover (e.g. scree slopes, rock slabs, summer firn, grass, etc.). For more information check out the
telemarktips.com forum and the
Mountain Conditions Report.