Snow Observations List

Winds started cranking this afternoon in the alpine and ridge tops. Lots of snow being transported around. Ski and skin tracks were disappearing close to the ridge between laps. 

ECTP 22 & ECTP 27, down 50 and PST 75/100 end, down 50 & 80 at 7800 ft on E aspects on the ramp above Bradley Meadows

PST 45/100 end, down 180 on E aspects at 7700 ft on E/NE aspects at N end of the top of Bradley Meadows 

Toured into Frazier Basin today and noted a few instabilities. First, on our approach, we experienced a loud "whumph" around 7000' on an East facing slope. Second, we saw a large natural avalanche above Ainger lake (E-SE facing) that ran from near the top of the ridge itself to propelling debris up, over, and past the lake. The crown ranged from 2-5ft high spanning 400-500ft across the face. Lastly, the wind was whipping and transporting lots of snow. As we gained a North-East facing ridge around 8500' a couple of pole/hand pits reviled a 4" pencil hard wind crust. Spring is in the air but it is still very much winter out here.   

Saw this crown from a distance today. Possibly natural R3-D3 on ESE aspect, likely caused by wind loading. Unsure when it occurred, but crown looked large and debris ran into the flats mowing down some small flag trees. 

We were forced to turn around yesterday on emigrant peak. We heard 2 large wumphs occur under our feet while skinning up and a visible crack was also seen. We dug a pit and obtained a score of 14 and it propagated all the way across the snow pack. The snow near the ground is very sugary and weak. This was on a SE facing slope at 7500 feet. 

My ski partner and I toured into Frazier Basin on Saturday, April 1st. We observed obvious signs of wind loading as we made our way up from Fairy Lake to the Frazier ridge. We found a crust layer a few centimeters thick that was widespread throughout the basin. The crust was not shooting cracks as we moved but hand pits showed that it was cohesive and easily breaking on the soft snow below. My ski Partner popped off a small wind slab that had enough energy to knock him off his feet. This was the only slab we found that moved after skiing three lines on different aspects. The wind slab that broke was just below a ridge in a bowl feature that probably experienced more wind loading than most other areas in the basin. We also observed an old avalanche at the end of the basin possibly from a cornice fall that ran the whole length of the slope down to the trees in the center of Frazier Basin. Overall it was not feeling like a spring snowpack and you should continue to be skeptical of multiple layers in the Bridgers. 

We were snowmobiling up portal creek today near the hidden lakes trailhead and I set off a small slide remotely by riding below a small ridge. The slide was about 3 feet at its crown 30 or 40 feet wide and ran about 40 yards. It just came down to where my track had crossed underneath. Everything was fine and we stayed safe and continued on with our plan and had a nice day.

This natural avalanche was observed in the afternoon around 1500. It was not seen earlier in the day and is thought to occurred at some point after 1200. It was seen from a distance on Pioneer mountain. It occurred on an E facing slope around 9600’. Active wind transport was noted on the ridge line above the avalanche. It looked to be around a R3-D2.

Toured in Beehive, Middle, and Bear Basins. In hand pits on W aspects we observed soft slab moving easily on a thin layer of facets over a melt-freeze crust buried about 40-50 cm. We dug on an E aspect at 9275' in Middle Basin and got ECTP24 on the same layer. Kept our objectives mellow. Did not observe any avalanche activity. 

After a long day of riding 2 to 3 thousand feet higher in good snow I was getting close to the truck after 10 or so miles on a mostly hard pack trail I decided to climb this hill in a split second decision. My sled was overheating and my plan was to cool it down. As I ascended the hill I hit a pencil hard wind slab about a third of the way up, I knew instantly that I was in trouble as this slope ended up being much steeper than I had initially thought. I made a decision in the moment to continue up the slope as it was not many vertical feet in elevation. My thoughts were that I had lots of speed and momentum built up and that that would carry me up I also thought that if I tried to make an aggressive turn it would put more stress on the snow pack and I also figured the closer to the top of the slab I was when it fractured the better off I would be. I made it about 100 feet from the top of the hill when it first fractured, I was about 20 feet from the fracture and there was a point slightly to my right that was the closest point of the fracture to me. I turned slightly right heading to the closest point of snow above the fracture line. As I turned the slope started sliding. The top of the of the slide rolled over like a large wave and a block hit me in the ribs luckily not nocking me off my sled. I maintained full throttle and kept my momentum traverseing through the rolling blocks. My only thought was to try to stay on top of my machine and keep forward momentum. In the last few moments of the slide I could feel I was loosing control of my machine because it was starting to get sucked into the avalanche. When the slide stopped I was in snow to my knee on my uphill side. I want to end this with a warning of complacency. I had been in big terrain all day and didn't analyze the slope like I should have a simple glance for a moment and I would have recognized the dangers of the wind slab. I got complacent and it almost got me injured or killed. Just because a slope is small doesn't mean it isn't dangerous.

**Reporting this from a friend of a friend. Not my photo, nor was I involved.**
 

one skier got caught above large bottom cliff, carried all the way down over cliff to the apron. Said skier walked away completely unharmed. Not buried. 
 

north face of that bowl, near cornrows. 

Additional info from BSSP: 

"There was a large, deep slab avalanche snowboard triggered in Lone Lake Cirque this afternoon. The
slide ripped in a secondary start zone below ridgetop, and ran far into the flats, and may have run a

bit uphill, where it encountered the rock glacier moraine in the runout. It looks to be a R4, D2.5."

From IG:

Think this was a recent natural up buck I saw today. Didn’t get close enough to see but looked like it was a big crown… down low 8900ish SE

Uneventful day. Rode through all three yellowmules, McAtee Basin, and the heads of Muddy and Bear Creeks. Saw no recent avalanches or other signs of instability. Dug two snowpits on E and N aspects at ~9400 ft. About 12" of snow from last weekend with 1.3" snow water equivalent. ECTN14&16 under the new snow. No other results.

Snowing lightly with overcast skies and calm winds. We'll be paying attention as it starts snowing tomorrow, especially if the wind picks up as forecasted. 

Via phone message:

A large natural avalanche occurred on the north summit of Bridger Peak yesterday (Monday, 27 March). The crown line was complex.

We rode into the Throne from battle ridge and skinned up the east face. We saw three new snow avalanches (previously reported) on the SE and E faces of the Throne where we parked the sleds. Surface crusts are quite variable depending on slope angle, aspect, and shading from trees. The crust was generally present and breakable on the SE and E aspects we traveled on. We dug a quick pit on at the base of the E face. ECTP16 on 1 mm facets underneath last weekends snow. We measured  50 cm (20") of new snow with 2" snow water equilavent.  Dug again in the crown of one of the slides. The new snow had consolidated a bit because of a more southerly aspect (~16" deep), but there was also 2" of SWE in the crown. Slide broke on small facets above a firm crust. The slides all appear to have run mid storm or just as it was ending. One of the slides was clearly skier triggered, the others are unknown.

The presence of facets under the new snow means that it'll take longer for that new snow to stabilize. 

On my walk up to divide today 3/28 I noticed a few small storm slabs that broke on the west side of the main fork of hyalite off the summer trail.  This area had similar storm slabs that broke back in mid February during a large storm 

up in the alpine there were no avalanches to report 

On a sunset tour we headed up to grab some low hanging fruit in the W Bridgers. We were shocked to find such a deep snowpack in the plains. Skiing a meadow off the valley floor from the North Cottonwood Canyon TH, we dug a pit at an elevation of approx. 5,800ft on a west aspect. The snowpack was 85cm deep, with this weekends new snowfall making up the top 45cm, the sun had affected the top 5cm creating a thin warmer layer and then surface crust as temperatures dropped. The bottom 40cm was a melted down, 4F hardness layer of weaker snow to the ground. At the moment the new snow appeared to be bonding well to the previous snowpack but it was very visible that this bottom layer was trending towards faceting and weakness. Our test result was ECTN 14. There was no breakage into the weak snow below the new snow. We skied a beautiful 25-30 degree pitch into the setting sun.

We observed evidence a couple of recent slab avalanches at the throne

From IG: Battle ridge today/yesterday the 27th. Noticed this and a few other smaller solar releases as well as a couple storm slabs from during the cycle. Sun crust formed rapidly and there was a lot of wind loading in the afternoon

We rode through to the Goose Lake wilderness area boundary and skied from there to look at the snowpack in higher elevation, alpine terrain. Like the day before, we managed our exposure to avalanche terrain be keeping ourselves off and out from under large slide paths because of our concern for the possibility of deep slab avalanches. 

We dug two snowpits on the tour and found a layer of surface hoar buried 20 CM deep (on the far end of Goose Lake at ~10,000' elevation on an east and northeast-facing slope). It did not propagate in any of the tests we performed, but it is certainly something to watch for. We did not see it in our snowpits yesterday, it will take more time and more snowpits to pin down the extent of this new weak layer and whether it will become a widespread problem. 

Our two primary concerns for today were wind slabs, we observed several recent wind-slab avalanches on Mount Fox and Henderson Mountain, and deep-slabs like the one that caught a pair of riders on Thursday on the SW side of Henderson.