The total snowpack depth at treeline is around a metre, The alpine snowpack is generally deeper, but likely variable with fat drifts and boney rocks, while most slopes below treeline are likely still below threshold depths for avalanches. Although weaknesses exist within the recent storm snow, the main snowpack feature is a rain crust buried early November and now down around 80cm at treeline as as deep as 1.5m in alpine areas. A weak layer of facets on top of and within 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. Widespread whumpfing and cracking on this layer has also been reported from the Whistler area. 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, glaciers, etc.). For more information check out the
telemarktips.com forum and the
Mountain Conditions Report.