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Avalanche Forecast

Archived

Nov 28th, 2025–Nov 29th, 2025

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Glacier.

The snowpack dwindles significantly below 1600m.

The combination of challenging exits and short days make it a good idea to start your egress early.

Confidence

High

Avalanche Summary

There has not been any recent natural avalanche activity reported in the last few days. Some riders are reporting sluffing in steep terrain.

Large fracture lines and debris are still visible from last week's heavy storm and associated avalanche cycle.

Snowpack Summary

A thin sun crust exists on the surface on steep solar aspects. Surface hoar is growing on the surface at treeline. 40-60 cm of recent storm snow sits on a rain crust that exists up to approximately 2200m.

Lots of alders, logs, rocks and open creeks await riders looking for turns below treeline.

Weather Summary

A ridge of high pressure gives generally stable weather conditions.

Tonight Clear periods. Alpine Low -10°C. Ridge wind light NE.

Sat: Mix of sun and cloud. High -5 °C. Light SE wind.

Sun: Sunny periods. Low -7 °C, High -5 °C. Light West wind.

Mon: Flurries, 6cm. Alpine High -7°C. Light SW wind.

Terrain and Travel Advice

  • Make observations and continually assess conditions as you travel.
  • Carefully evaluate steep lines for wind slabs.

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.