The recent storm snow seems to be settling out with no significant layers. Moderate winds from the SW-NE have built
wind slabs that may be sensitive to rider triggers. Areas that may host a wind slab problem are
lee slopes and behind terrain features (spines, gullies, ridgelines). Two crusts have been identified in the snowpack: one close to the ground that formed in early November down 170-200 cm and one around 90-140 cm below the surface, which formed in early December. Recent snowpack tests done on the December crust from the Harvey Pass Riding Area showed a moderate compression test failure, with a sudden collapse characteristic but inconsistent results. Testing done in the Crowsnest South Riding Area showed compression tests in the moderate range with non planar breaks. Its important to dig down and test the reactiveness of these layers in your local riding areas. This layer may be difficult to trigger, however typical trigger points are thin-thick snowpack areas, cross loaded gullies or around rocky outcrops. If triggered a large destructive avalanche may occur. The mid pack is generally well settled throughout the region.