Avalanche Forecast

Archived

Feb 7th, 2025–Feb 8th, 2025

Alpine

Natural avalanches unlikely, human triggered possible.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely, human triggered possible.

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

Purcells, Esplanade, Dogtooth, East Purcell.

Look for areas where the surface snow is soft and avoid areas where the surface snow feels dense or "slabby".
In very steep terrain loose surface snow could gain enough mass to be a problem.

Confidence

High

Avalanche Summary

Thursday: A few small wind slab avalanches on north and east aspects were triggered natural and by riders.
Wednesday: Northwest of Golden, a small (size 1) rider triggered wind slab avalanche was reported on an east facing, treeline slope. Just beyond the region boundary to the east, a size 2.5 remote triggered avalanche was observed. see the report here.

We expect unconsolidated snow will remain reactive to skier traffic in steep terrain. Carefully manage sluffing.

Snowpack Summary

25-45 cm of soft surface snow is faceting in sheltered terrain at treeline and below. This covers a layer of surface hoar buried in late January that may be as large as 15 mm in some places. The surface hoar sits on loose, faceted snow in shaded terrain, and a crust on steep slopes facing the sun.

In the alpine, exposed terrain is generally wind-affected, and there is likely no surface hoar included in the late January layer, just facets, old wind-affected surfaces, or a sun crust.

A weak layer of facets from early December is 60 to 120 cm deep.

The base of the snowpack consists of a thick crust with facets or depth hoar in many areas.

Weather Summary

Friday Night

Partly cloudy. 10 to 30 km/h west ridgetop wind. Treeline temperature -20 °C.

Saturday

Mix of sun and cloud with flurries. 20 km/h west ridgetop wind. Treeline temperature -17 °C.

Sunday

Mostly sunny. 10-20 km/h northwest ridgetop wind. Treeline temperature -16 °C.

Monday

Mostly sunny. 10 to 20 km/h north ridgetop wind. Treeline temperature -20 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

Be aware of the potential for remote triggering and large avalanches due to buried surface hoar.
Keep in mind that human triggering may persist as natural avalanches taper off.
Be especially cautious as you transition into wind-affected terrain.
Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

Problems

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.

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.