Snow Observations List

Touring from 6800' - 8800'  breakable crust - both directions! Lots of whumphing down low but then none above 84-8600'.  

From email: "We didn't see any avalanches on E Henderson or E Sheep with decent vis on the ride in. One large avalanche on a heavily wind loaded slope below a huge cornice north of Scotch Bonnet. That one looked like it broke deeper/in the old snow, about 100' wide. Also saw one wind slab on a small slope north of Long Lake. 14-16" deep, 20' wide, and within the fresh wind slab. "

We rode up Taylor Fork around Skyline Ridge towards Cabin Creek. We found 12" of new snow had fallen over the last 24 hours. With poor visibility, we were unable to see any recent avalanche activity except for a small recent avalanche that happened near Beaver Slide. This was right next to a much larger slide that Doug and Ian had seen on 02/14/2024. While riding back we had a good view of the backside of Skyline Ridge above us and again saw no recent avalanche activity. However, many slopes had been stripped by recent winds. Strong winds and a foot of new snow that fell onto a weak snowpack kept us off of and out from underneath steep slopes, and recent snow made for pleasant riding conditions. 

From IG message: “These are on the ridge between Miller Mtn and Sunset Peak on North aspect. All of the North facing ridge of Miller Creek up to Miller Mountain had similar slides too. The crowns filled back in overnight… The North facing ridge on Sheep Mtn slid as well, not sure on the trigger but a rider from another group send the following image of the Sheep slide“

Toured up the west side of Woody via Central Park approach. Moderate to high wind gusts at the ridge line. Skied a couple laps in variable conditions on Sub bowl and then returned to the West aspect for a lap down South Central . 

Traversed into the tube at tree-line roughly 9900’ and triggered a small wind slab. Crown was around ~1 foot deep and maybe 40 feet wide. Possibly stepped down a bit once in the tube and then ran for about 300 feet. 

HS-AS-D1-R1

Went up to the prayer flags today. On the ridge about 100yards below the flags I went to the end of the cornice and gave it a stomp. Triggered a windslab that propagated about 50 to the left. 
HS-ASc- D1-R1-I

The crown was roughly 1-1.5 ft deep in the most wind loaded area. 
Multiple slides have went on this slope already this year, some running a good distance down through the trees. 

We rode up the road to Henderson Bench and dug on a northeast facing slope at 9,670'. While digging it was clear how poor the snowpack structure was. It was difficult to dig through a 2 foot thick hard slab, but once through the slab I sunk to the ground through 1.5 feet of weak sugary facets. We had an ECTX. After some extra hits, removing 2/3 of the slab, and a few more hard hits, we got a dramatic collapse and propagation. The facets were F+ in hardness below a P+ hard slab. Although the weak layer was difficult to affect in this spot, finding the right spot on a slope to collapse the weak layer would produce a big avalanche, as shown by a rider triggered slide two days ago on Fisher Mtn.

We also rode up to Daisy Pass. Visibility was good enough to see most slopes, but in flat light. We didn't notice any new avalanches.

Snow was falling lightly (S -1). Overcast skies. Wind was moderate with frequent strong gusts out of the west-southwest, forming drifts along road cuts and convexities.

Saw multiple large slides around the McAtte drainage N/NE aspects. Some were larger than others but all ran on what looked like a persistent grain or even to the ground in some. Probably natural released over last few days.

During our time out the wind was hammering the ridge and clearing transporting and forming slabs. 

Several small slabs pulled out above The Shimmy, left of Cleo's. Observed from across the valley while climbing the Dribbles. Did not observe them run, only saw the crowns. Unknown date of avalanches, but crowns were quite distinct from across the way.

Lots of wind transport all day.

We rode to the south shoulder of Scotch Bonnet, then over Lulu Pass, towards Round Lake behind the north end of Sheep Mtn., and back to Lulu Pass. It was snowing very lightly and wind was blowing strong. Wind was blowing snow into drifts 6-8" thick on the leeward side of trees and convexities. We had intermittent ok visibility and could see old debris from last weekend on east Henderson, and we got a pretty good look at the slides on Fisher Mtn. that were triggered yesterday. They appeared 2-3 feet deep, and the debris was very hard. Crowns were already at least half drifted in.

We saw another slide on the north end of Sheep Mtn. on a slope above the steep chute where people climb out of Goose Creek (photos attached). This slide had not been reported previously and looked similar in age to the two triggered yesterday, so maybe broke naturally or human-triggered in last 24 hours. It broke near a scoured north facing ridgeline, 1-1.5' deep, 175' wide. HS-R3-D2-O.

We dug a pit on the south facing shoulder of Scotch Bonnet and had an ECTP24, down 1.5 feet, not on the previous layers of concern which were lower down (pit attached).

Regardless of stability test results or which layer slides are breaking on, recent avalanche activity and more wind-loading is enough evidence to avoid avalanche terrain.

Large slide in the north basin of fan mountain. The flies is below the north, north east couloir and the crown runs all the way around the basin. It went to the ground below the couloir and a few other places. 10ft crown probably at the biggest point below the couloir. 
 

no photos due to poor camera

Observed signs of a large avalanche along West aspect of Lionhead.  I am not sure when it occured.  At this distance and my experience level I can only estimate the crown at 3-4' and 1000'+ feet wide.  It appears to have run about 650' vertical feet and the runout zone goes all the way to Targhee creek into several terrain traps. 

We noticed that a widespread crust had formed at lower elevations from the recent warm spell, especially in areas without consistent shade. The snow that remained available for transport was easily being picked up by moderate to strong SW winds at treeline. Many tracks had been filled in by the wind transported snow, and a dense, hollow windslab was found in isolated spots.

The snow ranger crew was out in the Bridgers today, mostly lower down in the Throne and Naya Nuki areas.  The wind was very strong all day long and even in the woods our tracks were filling lightly from wind transported snow.  We could see a fair amount of snow blowing over the ridge top and some very textured looking snow higher up.  We did not see any recent avalanches.  

North facing aspect above McAtee creek.  Triggered one remotely while traversing below, ~150 yards away, and likely triggered the second one from below as well but cannot confirm. 4-6 foot crowns, 50-100 yards wide, ran 75-100 yards

One slide seems to be natural.

just around the ridge, lookers right, a snowmobile triggered slide

rider in photo. Rider was carried downhill, not buried. Very very lucky

the two slide seem to have happened at the same time

We skied Texas meadow this evening, and found relative stability. We tested a small hand out which did show the poor snow structures that the rest of the area with a very cohesive top on a sugary base, but we didn't find wumphing or other signs of instability in this zone. Southern aspects did have a strong sun crust on them, while others had great snow. There was also very gusty wind from the south which made temporary whiteouts and could be transporting snow. 

We rode up to the Indepedence Mine area (outside our advisory area) to check out the snowpack conditions before the Poker Ride this Saturday. As we arrived in the basin we saw a good sized recent natural avalanche. This really tells you all you need to know - recent avalanches are the clearest sign that triggering more avalanches is possible.

We then dug and confirmed that the snowpack is just as weak as it is across our advisory area. Two feet of fist hardness facets at the ground with almost four feet of slab above them make for a very weak structure.

If you're headed up for the ride this weekend I'd advise avoiding riding on and staying out from under slopes steeper than 30 degrees. 

We toured to the east shoulder of Divide Peak today, 02/22/2024. We saw several natural avalanches on the north-facing terrain in Divide Cirque, below Hyalite Peak, and Overlook Mountain. These avalanches likely happened following a storm near the end of last week. Near the base of Divide, we dug on a SE-facing slope at 9300' and had a stability score of ECTP30. From here, we continued up the shoulder, trying our best to stay on slopes near 30 degrees in steepness. At the top of the shoulder on an east slope at 9600', we dug another pit and found 133 cm of snow and had a stability score of ECTP20. In both our snowpits, we had a well-defined layer of weak faceted snow buried 2-3 feet deep. This is the layer our stability tests failed on. 

During our tour, we saw no cracking or collapsing, but recent natural avalanches near us and the large natural avalanche seen on Mt. Bole a few days ago encouraged us to keep our terrain choices conservative. We skied down near our skin track one at a time and avoided areas with terrain traps like gullies, cliffs, and thick trees below. 

My brother and I toured into the skillet at Bacon Rind. We dug a pit at the top of the skillet, east aspect, 9000 feet. Total snow depth was 115cm. We observed CT14 and ECTP25, 2.5 feet or 75 cm down, propagating on large old facets below a hard slab. That slab was dense and carrying some energy when collapsed in our column tests. We also observed multiple suspected week old natural avalanches on northeast aspects.