Deeply buried weak layers exist throughout the region and a cautious approach remains critical. Don't let the lure of powder pull you into bigger terrain.
Avalanche Problem 1: Persistent Slabs




- Good day to make conservative terrain choices.
- Be mindful that deep instabilities are still present and have produced recent large avalanches.
- Minimize overhead exposure; avalanches may reach the end of run out zones.
Avalanche Problem 2: Wind Slabs




New snow and wind on Thursday night and Friday are expected to form new wind slabs in higher elevation lee terrain. A surface avalanche in motion could be what it takes to trigger a deeper and more destructive persistent slab avalanche.
- Avoid lee and cross-loaded terrain near ridge crests.
- Be cautious as you transition into wind affected terrain.
- If triggered, wind slabs may step down to deeper layers and result in large avalanches.
Avalanche Summary
Reports from Tuesday reflect increased visibility over terrain that was obscured during Monday's storm. Evidence of a natural avalanche cycle involving each of our persistent weak layers was observed, with numerous avalanches reaching Size 3.5 and several crown fractures up to 3 metres deep. These are believed to be some of the deepest crowns in the region's historical record. Here's a great MIN post from Kootenay Pass that details some of the recent activity.
On Wednesday, explosives avalanche control in the mountains near Nelson triggered a handful persistent slab avalanches in the size 3-4 range at treeline and in the alpine.
Looking forward, expect newly formed wind slabs and the persistent slabs beneath them to remain reactive to human triggers with the potential for very large and destructive avalanches.
Snowpack Summary
During the last few weeks of January, storms brought around 100 cm of snow to the region. On Monday precipitation fell as rain below about 1300 metres and a near-surface crust may exist in some areas below treeline. Where more recent precipitation fell as snow, southwest winds may have formed touchy wind slabs in high elevation lee terrain.
The critical instabilities, however, are buried well below the surface. A mixture of weak surface hoar and/or a crust from mid-January is buried beneath all the storm snow at 80-110cm deep. Numerous recent avalanches to size 2.5 have been reported on this layer and large, destructive avalanches at this interface remain a concern.
Below this layer lies a second crust/surface hoar interface buried early-January that is now 110-130 cm deep. Several recent avalanches have stepped down to this layer.
The mid-December surface hoar layer is buried 120-150 cm below the surface. This layer has continued to produce step down releases and "sudden" test results. It is most pronounced at treeline, but is also present below treeline .
Weather Forecast
Friday: 10-15cm of new snow / Moderate westerly winds / Freezing level at 1400m
Saturday: Light flurries / Moderate northwest winds / Freezing level at 1500m
Sunday: 5-10cm of new snow / Light southwest winds / Freezing level at 1700m
Note: Confidence is low for forecast wind values and precipitation amounts for Saturday and Sunday.
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The snowpack is complex and continues to produce very large avalanches on several weak layers buried 80 to 150 cm below the surface. Moderate-angled, simple terrain selection remains critical to safe mountain travel.