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Avalanche Forecast

Archived

Feb 14th, 2026–Feb 15th, 2026

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

Regions

Glacier.

New snow and wind has built fresh windslabs, be cautious as you transition in to open terrain.

Keep the persistent slab problem on your mind at treeline and below - be especially cautious if you are exploring areas that don't see regular traffic.

Confidence

Moderate

  • We are confident that there are persistent slabs in the snowpack, but uncertain about how likely they are to trigger.
  • We are uncertain due to the variability of wind effect on the snowpack.

Avalanche Summary

On Saturday new snow and wind triggered a natural avalanche cycle. A field team observed a size 2.5 from the Frequent flyer path, which stepped down to the Jan 26th layer on the fan, as well as several size 2s from the N side of Cheops. There were also several size 1.5-2s in the steep terrain of the highway corridor.

On Friday, a team remotely triggered 2 size 1.5s between 1600-1850m, on the Jan 26th layer. This was in infrequently travelled terrain below the Avalanche Glacier.

Snowpack Summary

A sneaky 20-30cm of new snow fell Saturday, bringing this weeks totals up to 50-60cm.

Gusty alpine winds continue to build fresh windslabs in exposed terrain.

There are several crusts in the upper snowpack from the springlike temps and sunshine we've had in the past 2 weeks.

The Jan 26th layer of surface hoar, facets, and a crust, is buried down 45-80cm. The largest surface hoar is preserved in sheltered areas below treeline.

Below this the snowpack is well settled/strong.

Weather Summary

A week ridge brings clearing skies and valley fog.

Tonight: Clear periods. Alpine low -10°C. Light West ridgetop winds.

Sun: Sunny periods. High -10 °C. Freezing level (FZL) valley bottom. Light SW wind.

Mon: Isolated flurries. Low -11 °C, High -7 °C. Gusty moderate SW wind.

Tue: Flurries (3-5cm). Low -17 °C, High -9 °C. Light variable wind.

Terrain and Travel Advice

  • Look for signs of instability: whumphing, hollow sounds, shooting cracks, and recent avalanches.
  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Approach steep and open slopes at and below treeline cautiously, as buried surface hoar may exist.
  • Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.