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
Toured into divide basin on Friday. Looking at the north face of hyalite peak we saw a slide that went to the ground, and was about 150 feet wide. It possible this slide propagated further, but severe wind loading was actively occurring and it was hard to tell if the crown had been filled back in. We dug a pit at 9300 feet on a SÉ aspect and found a 80-100 cm HS and right side up snow pack with minor faceting below a crust 30 cm from the bottom.
Toured into divide basin on Friday. Looking at the north face of hyalite peak we saw a slide that went to the ground, and was about 150 feet wide. It possible this slide propagated further, but severe wind loading was actively occurring and it was hard to tell if the crown had been filled back in. We dug a pit at 9300 feet on a SÉ aspect and found a 80-100 cm HS and right side up snow pack with minor faceting below a crust 30 cm from the bottom.
This natural avalanche of wind blown snow narrowly missed hitting two skiers.
Photo: Anonymous
