Bridger Range

Mar 7 obs: "There was 6" of low density snow from yesterday.... The new snow was low density and sluffed easily on steep shady northerlies. On steep slopes facing the sun (south and east, and probably west) the new snow sat on a crust and became moist as the sun warmed it up and started to slide under skis. We saw a couple very small natural loose snow slides below rock outcrops on south facing slopes. Air temperatures were well below freezing, especially with wind chill, but the sun quickly warmed the recent new snow." Photo: GNFAC

We rode from Battle Ridge and skied up the east face of The Throne to look at the stability of the recent new snow.

There was 6" of low density snow from yesterday. Winds were stronger than expected, from the north at the top of the Throne, and increased through the morning.

We found fresh drifts that were reactive, cracking easily and 5-10' wide out from our skis, on south and east facing slopes around 8000-8300'.

The new snow was low density and sluffed easily on steep shady northerlies. On steep slopes facing the sun (south and east, and probably west) the new snow sat on a crust and became moist as the sun warmed it up and started to slide under skis. We saw a couple very small natural loose snow slides below rock outcrops on south facing slopes. Air temperatures were well below freezing, especially with wind chill, but the sun quickly warmed the recent new snow.

It is spring, in addition to assessing for unstable drifts of snow, plan for wet snow avalanche hazards to increase in likelihood throughout the day when the sun is out and temperatures are near or above freezing.

From obs on 3/4/25:

"Saw a few sluffs in the new snow triggered by skiers in the very steep terrain just north of the Bridger Bowl ski area boundary (see photo). These sluffs were small, definitely not large enough to bury someone."

Took a quite tour up The Ramp to see how the new snow is bonding. Found 3-5" of new snow. Non-cohesive and seemed well bonded to the surfaces beneath. No signs of wind effect. No slab avalanches or signs of instability noted.

Saw a few sluffs in the new snow triggered by skiers in the very steep terrain just north of the Bridger Bowl ski area boundary (see photo). These sluffs were small, definitely not large enough to bury someone.

Skies were still blue with increasing clouds when we rode up into Fairy Lake zone this morning. We popped up onto the Frazier Basin ridgeline and could see many tracks from skiers over the weekend. As we descended back to Fairy Lake and transitioned to skis, the cloud deck increased and the ceiling lowered. We ascended up Nayu Nuki's east shoulder and at times visibility was limited to 25' in front of our ski tips. Temps were still quite warm and winds were minimal. 

Snow surfaces were variable with a mix of sun crusts, wind board, and in shallower tree-sheltered zones, sugary faceted snow. It will be interesting to see how well a few inches of new snow this week bonds with these different snow surfaces. 

While our original trip plan involved stepping out into steeper avalanche terrain, we decided to pull the plug due to extremely limited visibility. This was an example of how even though avalanche conditions may be generally stable, there are other factors to consider when choosing to ski steeper lines (visibility of your partners, visibility of surrounding avalanche terrain, etc.) 

Observed multiple wet loose slides naturally triggering and running on south facing slopes beyond bradleys and on the south facing aspects of hourglass chute.

Observed multiple wet loose slides naturally triggering and running on south facing slopes beyond bradleys and on the south facing aspects of hourglass chute. Photo: T McGarry

Observed multiple wet loose slides naturally triggering and running on south facing slopes beyond bradleys and on the south facing aspects of hourglass chute.