Northern Gallatin

Surface boar forming in sunny spots at lower elevations

Pin wheels coming down on south facing road cuts

Backside skiing was already getting heavy just after 10, reasonably heavily trafficked since last storm, someone ski cut just below cornice with no movement.

Front side has a supportable sun crust under the last 4" storm

At 1:30pm on 11/23 I intentionally triggered a fresh drift of snow in a narrow avalanche path along the edge of the north bowl at Bridger. Northeast aspect at 7,600’ elevation. The crown was 6-8” deep consisting of snow that fell today, 20’ wide and ran 250’ vertical. SS-ASc-R2-D1.5-I. Photo: GNFAC

At 1:30pm on 11/23 I intentionally triggered a fresh drift of snow in a narrow avalanche path along the edge of the north bowl at Bridger. Northeast aspect at 7,600’ elevation. The crown was 6-8” deep consisting of snow that fell today, 20’ wide and ran 250’ vertical. SS-ASc-R2-D1.5-I. Photo: GNFAC

Big Sky ski patrol triggered these slides with explosives on 11/22 during routine avalanche mitigation work. The avalanches were hard slabs that averaged 12" deep and broke on a weak layer above a crust on top of snow that fell in October. Photo: BSSP

Big Sky ski patrol triggered these slides with explosives on 11/22 during routine avalanche mitigation work. The avalanches were hard slabs that averaged 12" deep and broke on a weak layer above a crust on top of snow that fell in October. Photo: BSSP

During our trek up to Narcolepsy and the Champagne climbs, we observed a large amount of surface hoar atop the snow. There were large (1/4-1/2”) flat crystals growing from the snow sitting on a small icy faceted layer. It seemed to be widespread and was found throughout most of the canyon. We figured this may cause instability during the next snow accumulation

During our trek up to Narcolepsy and the Champagne climbs, we observed a large amount of surface hoar atop the snow. There were large (1/4-1/2”) flat crystals growing from the snow sitting on a small icy faceted layer. It seemed to be widespread and was found throughout most of the canyon. We figured this may cause instability during the next snow accumulation.

En route to Narcolepsy, we encountered waist deep powder and very unconsolidated snow. Even higher up near the climb we did not find any evidence of wind slabs or consolidated snow. We did witness a small loose snow avalanche on a sun exposed slope with an obvious fan caused from the moving snow.

During our trek up to Narcolepsy and the Champagne climbs, we observed a large amount of surface hoar atop the snow. There were large (1/4-1/2”) flat crystals growing from the snow sitting on a small icy faceted layer. It seemed to be widespread and was found throughout most of the canyon. We figured this may cause instability during the next snow accumulation.

During our trek up to Narcolepsy and the Champagne climbs, we observed a large amount of surface hoar atop the snow. There were large (1/4-1/2”) flat crystals growing from the snow sitting on a small icy faceted layer. It seemed to be widespread and was found throughout most of the canyon. We figured this may cause instability during the next snow accumulation