Snow Observations List

Today I saw evidence of Multiple N-R2-D2-I avalanches in the fairy lake zone. All three were NE facing, around 8800’. 2 slabs in Fraizer basin and one in the basin to the south. All three looked to be from 3/3-3/4 storm cycle

We skied in the love chutes and Fraizer basin today with No collapsing or cracking. 

Toured up to the Cinnamon Mountain Lookout today. In a small meadow along the trail I got a small whumph, with a crack propagating out 5-10 feet all around me. HS was around 30-40 cm in this meadow. HS rose rapidly with elevation and I had no other large collapses throughout the day, but noticed some localized cracking in recently formed windslabs, and rapid warming of the snow surface in the sun all day. I dug a pit about 200' down from the summit, directly south facing, and got unremarkable test scores from a scary structure (full profile is in snowpilot). With the several warning signs I had seen, I chose to take my test results with a grain of salt, and ski a conservative line.

East face of Republic Mountain above Erma Mine Cabins. 8800 ft natural avalanche just below the ridge. 3-4 foot crown, Apx 100’ across, ran approximately 1000 feet down the creek bed. Appeared to be from earlier in the morning possibly when the avalanche slid off the north face of Republic, as it had a light dusting of snow over the debris. This start zone was just over the ridge from the North facing 9:14 am avalanche but I don’t think the start zones were connected. 

Toured up on the ramp yesterday. In wolverine bowl, another skier and I both popped small wind pockets (6” deep at the most) about half way done the slope on a north facing roll. We also saw lots of snow transport up high on the ridges all day, as well as some slight warming on direct south faces. 

Observation cam from IG.

While riding north of Cooke City today we observed a large debris pile southern end of Sheep Mountain. SE facing at ~9700'. With poor visibility, I couldn't see a crown but much of the path had been filled in by wind and the debris was covered with fresh snow, making it at least a few days old. This slope was remotely triggered earlier this year in January by riders from the bottom of the slope. 

We rode into the Taylor Fork past Consolation Hill and to the weather station at Sunlight Basin. Winds were strong through the morning and we rode in a ground blizzard in all the open meadows along the trail in. There was not much for obvious drifting on the road, but the snow was obviously going somewhere. Snowfall intensity varied from a trace to an inch per hour (S -1 to S2). The highest precipitation intensities occurred around 1-1:30 PM as we began our ride out. 

We did limp our way to the Sunlight Basin pit site in poor visibility and dug, but the wind, snow and light were such that we couldn't even visualize the bowl near the weather station. Digging a pit, we found more of the same structure that we have tracked for a few months now. The depth hoar does not seem to have gained any measurable strength, but the layers of surface hoar are somewhat more decomposed. We got an ECTP 23 on a layer of facet in the mid-snowpack and an ECTP27 on the depth hoar. 

As we discussed in our video for the day, today and tomorrow the equation is simple... new and wind-drifted snow on a weak snowpack equals dangerous conditions. As we move into a period of high pressure for the rest of the week, the likelihood of triggering an avalanche will decrease as will signs of instability and, most likely, the frequency of avalanches. However, the consequences of getting caught will remain unchanged. As folks are enticed by steeper terrain later in the week, we strongly recommend an incremental approach to expanding terrain selection and avoiding slopes with terrain traps. Additionally, safe travel practices become essential if you are stepping into the ring, especially carrying rescue equipment, knowing how to use it, and traveling one at a time on any slope steeper than 30 degrees. 

From IG:

Very large natural avalanche in the Lionhead Area. Multiple other smaller naturals as well.

Pics taken 03/05/24

We toured up toward the Skillet along the standard uptrack route at Bacon Rind. We deviated to the south to look for a natural avalanche that broke on March 2nd in the south-facing meadows a third of the way up. We did not find it but dug a pit. 95 cm HS with a newly buried weak layer of facets above a crust at 52 cm (ECTP22x2 plus an ECTN17 on this layer). The depth hoar near the ground was moist. 

Somewhat dejected after failing to locate the avalanche, we proceeded back to the typical route. We came across a deep avalanche on a small rollover. 100 feet wide, 3-4 feet deep, and 50-75 feet vertical. Slope angles ranged from 29-33 degrees steep. It was an R5, D1.5 avalanche that certainly would have been very dangerous on a larger slope. ECT in the crown was unremarkable (this is not uncommon in the crown of an avalanche), PST 30/110 End. 

Continuing up, the next open meadow had collapsed and was splintered with shooting cracks. The failure propagated through the trees with more cracks and buckle marks as the slab tried to release... which it did a bit further downslope. Again, the crown was 3-4 feet deep, and the terrain constrained the length. 

No additional signs of instability. 

These two avalanches were different than the two we were initially looking for. I suspect skiers triggered them remotely on March 2 given the amount of new snow on the debris, but they may have failed naturally. Regardless, avalanches in these locations are very unusual and are indicative of dangerous conditions. With more snow coming the next two days, travel in or near avalanche terrain requires a great deal of caution. Conservative terrain selection will be essential. 

Observed a debris pile on the east face of Fischer Peak. Unable to determine when and what triggered it. Numerous debris piles on the Rasta Chutes on Scotch Bonnet. 

The Snow Ranger crew was out on Buck Ridge today.  We did not see any new slides around Beaver Creek, 1st Yellowmule, or Slatts Hill/ upper Buck Creek.  It began snowing before we made it to the McAtee/ 3rd Yellowmule area but from what we could see, it looked like the N/NE faces in McAtee that slid just over a week ago had avalanched again, nearly to the ground.  There were slightly dirty looking debris piles mid slope and several prominant crowns just below the ridge top but it was hard to make out details through the light snow, even with binoculars.

While traveling to Big Sky from Ennis, I noticed a large avalanche on the east face of Fan Mt.

Crown appears to start at approx. the 9500' elevation with a vertical drop of at least 2000'.  Crown appears to be 200-300 yards wide

White touring in the History Rock area, I spotted a couple of recent slides on the NW shoulder of Mt. Blackmore. From a distance, these look like dry-loose slides on the recent snow interface around 8,500ft. on a N-NE aspect.

Otherwise, 12-20cm of new snow was present in the area (~ HS 80-115cm), with evidence of wind loading on east aspects, and scouring on west aspects. No other signs of instability were observed.

Shot from the top of Flanders, ~1400 this afternoon, 3/3/2024. Big slide(s) on Arden and in Maid of the Mist.

Looks like the skin track and ski track between the two slides got taken out. At first glance from across the way it looked like the skin track was crossing over the debris, but when zoomed in it looks like the debris overran the skin track and the ski track.

From email: "Two big avalanches observed above the “plug” east of Cooke city. on my ride over this AM. One ran to the road, unclear if it went over it and maybe the groomer ran over the debris. Appear natural or possibly snowmo triggered? " 

We rode near the Throne today 03/03/2024. From the truck driving up and down canyon, we saw several natural loose snow avalanches that broke beneath ridgelines and one slab avalanche near Bridger Peak. While riding into the Throne we saw a large natural avalanche south of Ross Peak that likely happened early this morning. Many slopes steeper than 30 degrees had numerous natural and a few human-triggered slough avalanches that entrained storm snow from the last 24 hours, some also entraining snow that fell on Friday as well. These avalanches were large enough to bury a rider or skier. 

Near the throne on an east-facing slope at 7300', we dug a snow pit and found 23" of new snow that had fallen since Friday equaling 2.1" of snow water equivalent. 14" inches of this fell late last night (0.75" of SWE). Our stability tests yielded ECTN12 results below the new snow. Recent snow made up a little less than half of our snow pit height (HS 133 with 54 cms of new snow since Friday). 

Wind remained calm today where we rode, but all day we saw snow being transported at the ridgeline above. Storm totals were well distributed and at all aspects and elevations we rode we found roughly 20" of recent snow. 

From IG on 3/3/24. Natural on Wolverine and natural between Miller and Sunset. Looked like they went today or yesterday.

We saw one avalanche on a southeast facing slope. At about 7,400’ on a North facing slope we experienced a valley shaking whumpf while traveling up a heavily used ski track. 

Remotely triggered a large avalanche on a N aspect at 9500 ft while ascending a ridge line [in Mill Creek, Absaroka]. We estimated the slide to be D3 R3. The crown spanned roughly 1400ft +/- and ranged between roughly 1-5ft deep. They appeared to be 2 distinct layers in the crown profile, one of recent ‘storm’ snow and a lower one above old facets. This was observed from a distance. Witnessed large trees being shaken by the slide and smaller ones completely breaking. The bottom of the run out became much more planar indicating the sheer volume of debris that filled in. Extremely powerful to witness such energy and destruction. All persons in the party were in safe terrain with no intention to ski this slope at all. 

Noticed the pictured recent avalanche on an east facing aspect in the alpine of Beehive Basin. I would estimate it at a D2 size slide. It seems to have been naturally triggered by cornice fall and likely stepped down to older faceted snow deeper in the snowpack.