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Avalanche Forecast

Archived

Mar 13th, 2025–Mar 14th, 2025

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

Regions

South Rockies, Akamina, Crowsnest North, Crowsnest South, Elkford East, Elkford West.

For best riding and lowest hazard, seek out low-angled, sheltered terrain where the snow hasn't been wind-affected.

Confidence

Moderate

Avalanche Summary

A few small size 1 wind slabs and loose dry avalanches were observed in the Crowsnest on Thursday. Snowpack tests done by our field team east of Elkford suggest that the persistent weak layer remains triggerable. Avalanches on the persistent weak layer are becoming less likely to trigger, but if they do, they can be large and highly destructive.

Recent reports have been limited. If you are visiting the backcountry, please consider submitting a MIN report.

Snowpack Summary

Recent snowfall of 5 to 10 cm has likely formed fresh wind slabs near ridgetops on leeward slopes facing north through east, driven by Thursday’s southwest winds. Below 1900 m and on sun-exposed slopes, the new snow rests atop a surface crust left by previous warm temperatures and solar exposure.

The region’s overall shallow snowpack is defined by a persistent weak layer of surface hoar or facets from late January, now buried 40 to 80 cm deep. This layer triggered large avalanches earlier in March, and remains reactive in snowpack tests. The greatest concern lies in areas where a thick, supportive crust is absent near the surface, increasing the potential for instability.

Weather Summary

Thursday Night

Mostly cloudy, with 0 to 2 cm of snow. 20 to 30 km/h southwest ridgetop wind. Treeline temperature -7 °C.

Friday

Mostly cloudy, with trace amounts snow possible. 15 km/h southwest ridgetop wind. Treeline temperature -4 °C.

Saturday

Mostly cloudy, with up to 5 cm of new snow. 10 to 20 km/h southwest ridgetop wind. Treeline temperature -3 °C.

Sunday

Mostly cloudy, with up to 4 cm of snow. 15 to 20 km/h southwest ridgetop wind. Treeline temperature -3 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid steep, rocky, and wind-affected areas where triggering slabs is more likely.
  • Be mindful that deep instabilities are still present and have produced recent large avalanches.
  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Choose low-angled, sheltered terrain where new snow hasn't been wind-affected.

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.