Total snowpack depth are probably close to a metre in most treeline areas and deeper but more variable in the alpine, while below treeline areas are probably still below threshold depths for avalanches. Recent reports include hard shears within the upper low density snowpack and continued wind slab development from northerly and easterly winds. Weak facets have been found near the base of the snowpack, with an associated crust in some areas. Check out the
Skeena/Babine discussion forum for more information.