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Avalanche Forecast

Archived

Apr 4th, 2026–Apr 5th, 2026

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Kispiox, Microwave-Sinclair, North Bulkley, South Bulkley, Telkwa.

Monitor recent wind loading patterns to move around new wind slabs. Choosing moderate-angled slopes with uniform coverage is a good way to avoid both surface slabs and deeper problems.

Confidence

Moderate

  • We are confident that there are persistent slabs in the snowpack, but uncertain about how likely they are to trigger.

Avalanche Summary

There was a remote-triggered wind slab in the Seaton area on Friday. Check out the MIN report here. Similar slopes should be eyed up critically.

On Tuesday, the field team saw a cornice-triggered size 3 persistent slab (NE aspect). It ran to valley bottom and is a good example of the persistent problem affecting the region. There have been no other recent report of avalanches, but observations are limited.

If you are heading out, post a Mountain Information Network report!

Snowpack Summary

About 15 cm of snow from the past few days has been redistributed by strong southwest winds, creating wind-affected surfaces and wind slabs in exposed alpine and upper treeline terrain. In more sheltered areas, the new snow has buried 20 to 40 cm of older faceted snow. This should be settling increasingly well with recent mild temperatures. On steep solar aspects, particularly below 1700 m, the new snow likely sits over sun crust.

A thick crust from late January can be found at a wide range of depths, from 75 to 150 cm. Where it is shallowest, facets are most likely to exist above it, and the more problematic it is expected to be.

We do not have concerns about the snowpack below this layer.

Weather Summary

Saturday Night
Mostly cloudy with scattered light flurries and a trace of new snow. 15 km/h southeast ridgetop wind. Treeline temperature around -3 °C.

Sunday
Increasingly cloudy with flurries increasing near end-of-day bringing an initial 1 to 2 cm of new snow, light rain below about 1200 m. 15 to 20 km/h southeast ridgetop wind, increasing. Treeline high temperature -1 °C as freezing level climbs to 1300 m.

Monday
Mostly cloudy with some clearing near end-of-day. Increasingly wet snowfall bringing 15 to 30 cm of new snow to higher alpine, diminishing with elevation to mainly rain below about 1200 m. 40 km/h southwest ridgetop wind. Treeline high temperature 0 °C with freezing level starting at 1500 to 1600 m and falling over the day.

Tuesday
A mix of sun and cloud after overnight flurries finish with about 5 cm of new snow. 20 to 50 km/h northwest ridgetop wind, easing. Treeline high temperature -2 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • The best and safest riding will be on slopes that have soft snow without any slab properties.
  • Be aware of the potential for large avalanches due to buried weak layers.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.