From IG message: “Buck ridge, snowmobile triggered avalanche. Propagated storm slab.”
Explored slopes in lower Hyalite Canyon between 6000-7000 ft in elevation. Really close to being skiable and good. Otherwise, we found snow depths ranging from 6 inches to 2 feet. Generally very weak and faceted with thick crusts on slopes with a southerly tilt. All this weak snow probably won't be an issue because this area only gets the scraps from storms and never has enough loading to make an avalanche problem.
Went into the beehive area today to do a bigger jaunt into the alpine and make it around the basins. Dug at 9200’ on an E aspect on the Beehive/Middle ridge and ripped two ECTs. First test result was ECTN12 on the dust layer. Second test yielded an ECTX. We went ahead with our plan to ski some fairly steep terrain throughout the basins, taking it slow, and making surface and visual observations throughout our day confirming our plan. Most of the surface snow was minimally wind affected and skied great. We saw only small sluffs on anything we could see (no slab avalanches). There was some small shooting cracks while setting skinners, but nothing especially concerning. There was evidence of a stubborn older wind slab underneath the newest snow on one of our lines. Overall, great day!
Today, we traveled up the Deer Creek drainage north of Big Sky. We experienced no cracking or collapsing and saw no recent avalanches. We dug in the snow on a S aspect at 7680' with unremarkable results. We dug again on a NE aspect at 8200' and got an unstable test result (ECTP 28) on surface hoar and near-surface facets buried under a 2' slab (F - 1F+ hardness).
A few keys points from today:
There are a lot of abnormal, mid to lower-elevation zones out there holding great snow and riding conditions - just remember that there are still terrain and snowpack features to be on the lookout for and avoided. Step off the skin track, look out for signs of red flags and dig down to see what is going on beneath your feet before committing to ascending or descending steep slopes.
Started touring from the road around 8:30, with temps just above 0F. Half an hour later and 200 feet higher (~6150 feet) we were down to base layers and temps were above freezing. The top 5cm of surface snow was moist for most of our tour, with about 15-20 cm of dry snow below, overlying a buried crust in most areas.
As we got higher (~7000 ft) we noticed roller balls from the previous day, as well as dust on the snow surface.
Above 8000 feet surface snow became mostly dry on northerly aspects but a surface MFcr or a thin layer of moist surface snow still existed on southerly aspects. We skied a northly aspect first and it wasn't too bad.
Around noon graupel showers turned into S2 snowfall with sustained strong winds at ridgetop. A very abrupt change in weather and snow conditions. As we descended and drove back to Bozeman the temperature inversion was still going strong.
Our main thoughts are that this bodes for weird things to come. The snow yesterday was falling on a crust at higher elevations, but burying cold (potentially faceted?) snow at lower elevations. There were signs of developing wet snow problems at higher elevations but mid-winter conditions at lower elevations. It seems like our standard way of thinking about avalanche problems/hazard distribution may have to become inverted along with the temperatures.
Swift Current lift shut down all day Wednesday 2/5/25 by ski patrol
Swift Current lift shut down all day Wednesday 2/5/25 by ski patrol
