Recent storm snow may remain reactive on wind-loaded terrain features and where it sits above crusts.
Avalanche Problem 1: Storm Slabs




- Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.
- Use caution in lee areas in the alpine and treeline. Storm snow is forming touchy slabs.
- Pay attention to overhead hazards like cornices which could easily trigger slabs.
Avalanche Summary
On Monday, natural avalanches up to size 2 were reported in alpine terrain while skiers and explosives triggered several size 1 avalanches at lower elevations. The 20 cm of new snow was poorly bonding to the crust and produced slab avalanches in wind-affected terrain and loose dry avalanches elsewhere.
On Sunday, small loose dry avalanches (size 1) were reported in steep terrain and one size 2 wind slab avalanche was triggered with explosives on a north aspect at 2100 m.
On Saturday, a large slab avalanche was triggered in the west of the region. See this MIN post for a photo and more details. A small wind slab avalanche at treeline was also reported.
Snowpack Summary
15-25 cm of snow on Sunday night has fallen above a melt-freeze crust on sunny aspects and all aspects below 1700 m. The new snow has been wind-affected and may take awhile to bond to the crusts.
A surface hoar and crust layer buried mid-March is found around treeline at a depth of about 80 cm, with weak surface hoar on northerly aspects and the crust elsewhere.
Deeper in the snowpack, the late-November weak layer is composed of sugary facets around a crust, which is buried around 200 to 300 cm deep and is currently dormant.
Cornices are large along ridgetops and were actively failing last week.
Weather Forecast
TUESDAY: Mix of sun and cloud with some light flurries (accumulations of 1-3 cm), moderate west wind, alpine high temperatures near -6 C, freezing level up to 1200 m.
WEDNESDAY: Increasing cloud, light to moderate southwest wind, alpine high temperatures near -4 C, freezing level up to 1400 m.
THURSDAY: Light flurries with 5-10 cm of snow, moderate southwest wind, alpine high temperatures near -8 C, freezing level at 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.
Storm slabs, as well as loose snow in sheltered areas, are not bonding well to underlying surfaces and will likely remain reactive. Large avalanches are possible on wind-loaded slopes.