New and old slabs are taking their time to bond to underlying layers. Be cautious on southerly aspects when the sun is out -- it could weaken the snow and trigger avalanches.
Avalanche Problem 1: Storm Slabs




- Use caution above cliffs and terrain traps where small avalanches may have severe consequences.
- Observe for signs of instability, such as cracking, whumpfing, and avalanche activity.
- Approach lee and cross-loaded slopes with caution.
Avalanche Summary
On Saturday, a large persistent slab avalanche was reported in the north of the region, failing on the early-March weak layer described in the Snowpack Discussion. It failed on an easterly aspect around treeline. Portions of the avalanche stepped down to sugary facets near the bottom of the snowpack.
Otherwise, there was further evidence of the natural cycle that occurred on Friday within the recent storm snow, with storm slab and loose dry avalanches. They were small to large (size 1 to 2.5), on all aspects, and at all elevations.
Snowpack Summary
Expect to find a surface crust on southerly aspects from the weekend’s clear skies.
A reactive slab about 50 cm thick has developed from last week’s storm snow. This slab overlies two layers of weak surface hoar, which exist on shaded aspects at high elevations. The slab sits on a melt-freeze crust on all aspects below treeline. The storm snow may still be loose in sheltered and shady locations.
Near the bottom of the snowpack, weak and sugary facets are found in shallow, rocky snowpack areas. Storm slabs have stepped down to these facets recently, producing very large avalanches.
Weather Forecast
MONDAY: Partly cloudy, light southerly winds, alpine temperature -12 C, freezing level 400 m.
TUESDAY: Mostly cloudy with light snowfall, accumulation 2 to 5 cm, light to moderate southerly winds, alpine temperature -11 C, freezing level 500 m.
WEDNESDAY: Mostly cloudy with light snowfall, accumulation 1 to 3 cm, light southerly winds, alpine temperature -10 C, freezing level 500 m.
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
- Northwest Inland URL:
http://www.avalanche.ca/api/forecasts/northwest-inland.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.
Recent storm slabs are found in the south of the region and older slabs exist in the north. Very large avalanches have occurred, as the snow is not bonding well to underlying layers of surface hoar, crusts, or sugary facets in thin snowpack areas.