Wind slabs, cornices and deeply buried weak layers are making for tricky conditions. The best approach is to choose conservative terrain, minimize your exposure to overhead hazards and avoid wind-loaded areas.
Avalanche Problem 1: Wind Slabs




- If triggered, storm slabs may step down to deeper layers resulting in large avalanches.
- Watch for whumpfing, hollow sounds, shooting cracks or recent avalanches.
Avalanche Problem 2: Deep Persistent Slabs




Large avalanches have been running on deep weak layers. Wind loading, fragile cornices, and smaller avalanches are all possible triggers, as well as thin or rocky snowpack areas where human triggering may also be possible.
- Avoid steep convexities or areas with a thin or variable snowpack.
- Be aware of the potential for large, deep avalanches.
- Avoid exposure to overhead avalanche terrain, large avalanches may reach the end of run out zones.
Avalanche Problem 3: Cornices




Cornices have triggered very large avalanches recently. Be especially wary of long runout distances in avalanche paths, and the possibility of mature timber being taken out by a surprisingly large avalanche.
- Avoid steep slopes below cornices.
- Give cornices a wide berth when traveling on or below ridges.
Avalanche Summary
Thursday natural storm slab and loose storm snow avalanches up to size 1.5 were reported to have occurred overnight with active loading during the storm.
Explosive control work and ski cutting on Wednesday produced widespread storm slab results up to size 2, between 1600-2100 m.
On Tuesday skiers were able to cut size 1.5 wind slabs on north east features at treeline. Wind slabs to size 2 were also reported, starting at the base of steep head walls.
On Saturday we received reports of impressive sizes of cornice chunks breaking off a tree line ridge feature near Harvey Pass (Flathead area), running far into the forest and meadow below. See here for photos.
Avalanche activity on deeper layers has tapered off for now, but it's best to avoid likely trigger points such as thick-to-thin snow pack areas and also close to the base of rocky headwalls.
Snowpack Summary
About 30-40 cm of new storm snow and wind have created wind slabs at upper elevations. This new snow overlies old wind slabs on leeward slopes at treeline and above, and a mix of surface hoar, facets and sun crusts on solar aspects.
Below 1700m, the new snow covers a rain crust from last Wednesday.
For the past month there has been regular avalanche activity on multiple weak layers in the mid and lower snowpack. A widespread weak layer from mid December composed of facets, crusts, and surface hoar is 120-160 cm deep. Also, a rain crust with sugary facets buried in late November is near the base of the snowpack.
The take home message is that several weak layers are still lurking in the snowpack and they deserve a lot of respect. Conservative terrain use is recommended while avoiding all overhead hazard.
Weather Forecast
TONIGHT: Cloudy with clear periods, light flurries. Accumulation trace. Ridge wind moderate to strong, southwest. Temperature -10. Freezing level valley bottom.
FRIDAY: Cloudy with sunny periods, light flurries. Accumulation trace. Ridge wind moderate, west. Temperature -5. Freezing level valley bottom.
SATURDAY: Snow. Accumulation 20-30 cm. Ridge wind light to moderate, east. Temperature -6 C. Freezing level valley bottom.
SUNDAY: Mainly cloudy, light flurries. Accumulation trace. Ridge wind light to moderate, east. Temperature -17. Freezing level valley bottom.
Avalanche Forecasts in your Inbox
Avalanche Canada has switched to an RSS feed for its daily forecasts. This is a much more flexible method that allows automatic delivery to your email inbox, or to an RSS reader of your choice.
What are RSS feeds?
RSS (Really Simple Syndication) is a popular standardized file format allowing up-to-date delivery of web-based content. RSS feeds enable you to receive content updates from websites, delivered to your email through an RSS aggregator (such as blogtrottr.com) or viewed through applications called RSS readers (such as feedly.com).
Set up an RSS feed for your email:
Select a RSS aggregator
- Lizard Range and Flathead URL:
http://www.avalanche.ca/api/forecasts/lizard-range.rss - Copy the url and paste it into the appropriate field of your RSS aggregator.
- Fill in your email address.
- Voila! Watch the Avalanche Canada forecast roll into your inbox.
Forecast Disclaimer
Avalanche Canada's Public Avalanche Bulletin, and other information and services provided by Avalanche Canada, are intended for personal and recreational purposes only.
**THIS INFORMATION IS PROVIDED "AS IS" AND IN NO EVENT SHALL THE PROVIDERS BE LIABLE FOR ANY DAMAGES, INCLUDING, WITHOUT LIMITATION, DAMAGES RESULTING FROM DISCOMFORT, INJURY, OR DEATH, CLAIMS BY THIRD PARTIES OR FOR OTHER SIMILAR COSTS, OR ANY SPECIAL, INCIDENTAL, OR CONSEQUENTIAL DAMAGES, ARISING OUT OF THE USE OF THE INFORMATION.**
The user acknowledges that it is impossible to accurately predict natural events such as avalanches in every instance, and uses the data in this bulletin with this always foremost in mind. The accuracy or reliability of the data is not guaranteed or warranted in any way and the Providers disclaim liability of any kind whatsoever, including, without limitation, liability for quality, performance, merchantability and fitness for a particular purpose arising out of the use, or inability to use the data.
New snow and wind have formed wind slabs in wind exposed areas at upper elevations in the Fernie area. This new snow overlies a variety of old surfaces including hard wind scour, old wind slab, and crusts.