Snow Observations List

Did a full profile while out in Goose Creek today. Results indicated poor stability on a NE aspect about 7200 ft. The primary layer of concern was the buried surface hoar layer roughly 30 cm down in this location, took moderate strength (ECTP18) to get full propagation. Skiing conditions were good in the new snow from this weekend, you could subtly feel the MF crust from the time before the recent storm. We observed a small layer of surface hoar this morning, that will most likely be destroyed today from the intense sun on solar aspects. 

Our group did a big loop - Daisy- wolverine- goose - sheep -lulu. Saw minimal wind transport except on high points ( see photo). After looking all day saw an R1D2 slide (see 2nd photo) on a ENE slope above 10,000' south of Lulu pass, unknown trigger, though the whole area around the slide had cornice growth. We observed a lot of tracks highmarking into windloaded alpine slopes but saw no rider triggered avalanches. 

We rode into the head of Cabin Creek from Taylor Fork and turned around behind Sage Peak, then headed to the northwest side of Carrot Basin at the wilderness boundary. We did not see any recent avalanches. We dug two pits. One at the wilderness boundary and one off the north facing ridge in Carrot Basin. At the wilderness boundary HS was 140cm and we had ECTN24 on surface hoar/facets buried 40 cm down. We also had an ECTP14 on facets near the ground, but this one seemed more like an outlier. In our pit at Carrot Basin HS was 155 cm and we had ECTX. Overall, stability seemed to be good. With minimal recent snow, and weak layers becoming stubborn, the likelihood of avalanches is trending towards unlikely.

On our 3rd lap on the North Side Burn in Sheep Creek, we traveled up the ridge to take a look at the steeper terrain to the west along the ridge. From our protected vantage point, we could see a recent wind slab that appeared to release naturally some in the past 24 hours. The crown was obscured, but I would code the avalanche as SS-N-R1-D1-S. The avalanche was approximately 3-6" deep, 25' wide, and ran for ~60'.

This afternoon my group of 4 was riding up out of Tepee Creek heading towards Cabin Creek and I set off this small slide on a northeast facing slope as I was coming down it. The slide broke about a foot deep on top of the packed layer of snow and was 150-200' wide at the crown. Thankfully it slid slowly, less than 100' and I was able to ride out of it. 

There was 9” of new snow at higher elevations compared to 4” at the parking lot, and what was accurately reported at Shower Falls SNOTEL. We saw strong winds blowing huge plumes of snow off Maid of the Mist proper. Spindrift and wind-loading into gullies, near ridgelines and other slopes exposed to the wind was our primary concern. We dug two snowpits, one in the Basin low on a north facing slope and another on the south-facing shoulder. We got ECTNs in both. We found the 2-3" thick layer of facets and surface hoar on the south-facing pit buried 3' deep. They propagated failure with a few extra hits in our ECT. They weren't sensitive where we dug today, but I would not forget about them. 

We avoided wind-loaded slopes entirely and would recommend digging down three to four feet to test the upper level of the snowpack before considering any steep slopes. 

The 3-5” of new snow at Buck Ridge has blown into 1-1.5’ wind slab throughout the area. Cornices were built along the trail, and along ridgelines. The wind continued to transport snow today. We rode towards Beaver Creek to see if there was any avalanche activity–we saw a few small wind slabs. Next, we headed to the head of Bear Creek. The snow had built big pillows of wind drifted snow along the climb to the wilderness boundary. We observed some cracking on this slope when we stepped off our sleds. We stopped and dug a pit on the east facing slope at 9,400’. We found 7.5’ of snow (240 cm), and we had an ECTP 14, 2.5 feet below the surface of the snow on a layer of facets.

From FB: Had some tourists in the shop trigger an avalanche on two top yesterday. Didn't get exactly where or much details. Steep tracked up slope they set off. Just a partial sled burial.

We toured up to the bacon rind ridge, descended a southwest aspect, and then headed over and up to the Ernie Miller Ridge.

In sheltered locations, there was approximately 15 cm of storm snow from Sunday into Monday.  

On an east-southeast aspect off of Ernie Miller between approximately 9000-9700', we found widespread 20-25 cm thick 1F wind slab sitting on 1 mm facets. The slab was moderately resistant in hand shears and remained intact once isolated. It was not reactive to our jumping on small test slopes. We observed no cracking during our ascent and saw no signs of reactivity during our descent.

Above approximately 9700', the surface was largely scoured and there was a thin wind skin.  

We observed similar facets below the storm snow on our ascent of a southwest aspect between 8000-8700' on the way back up to the bacon rind ridge.   

We rode up Yale Creek and into Mt Jefferson Bowl. Walking to the edge we triggered an avalanche (intentional) on a slope that was getting wind-loaded. It broke up to 1.5 feet deep, 250 feet wide and 50 feet vertical. The new wind drifts were sensitive to triggering and the slabs propagated wide. Weak layers at the old snow surface may have helped us remotely trigger the slope. The two things to look out for in the Centennials are weak layer of sugary snow or feathery surface hoar in the upper 3 feet of the snowpack and slopes that are freshly wind-loaded.

Dug a quick test pit on Tuesday on an E aspect in Middle Basin. Found that persistent weak layer we’d been worried about, but got an ECTX when we tested it. We railed on it pretty hard afterwards and finally got it to break. When it did, it propagated cleanly all the way. Looked like it didn’t quite have enough load to fail yet but it’s still set up to and maybe this storm that just rolled through brought that load. We did also see evidence of an old avalanche on an E aspect in Beehive basin. Looked to be a couple of days old, probably from before Monday’s storm. 

One maybe two distinct seemingly natural large natural slab avalanches on small slope directly next to bridger canyon drive.  One on the lookers left was likely cornice triggered, but on the right it's unclear to me if it propagated or released naturally.

A slide occured at cliff lake up the  North Meadow area. I realized it had blown half way out into the lake. Looked like 48 to 72 hours ago but ice had been comprimised pushing chunks up.

From FB: We saw a fresh break on the west face of sage peak last night, I would guess around 9500’.

We rode north of Round Lake this morning (2/6/23). Near Long lake we measured 9" of new snow = 0.55" snow water equivalent. Near the Goose Lake wilderness boundary we measured 10" new snow = 0.65" SWE. In places there were 1mm facets below the new snow.

Wind was moderate-strong at the ridgelines, but calm around the lakes. 

There was a small snowmobiler triggered slide on a convex bench between Sheep Mtn. and Round Lake that was triggered this afternoon. It was 1.5-2' deep, 30' wide, and looked to have broke on a weak layer below last week's snow, on a freshly wind-loaded slope. In a relatively shallow, rocky area (photo attached).

We rode up Yale Creek to across from Arange Peak, then back into Yale Creek. We dug 3 snowpits looking for weak layers and found them a foot or two under the surface. Feathery surface hoar mixed with small, sugary facets were found in all. This layer was not propagating in our tests, but we know that nearby in Lionhead they avalanched. We are not completely trusting of these layers, especially at higher elevations where wind drifts would be adding even more weight to these layers.

This afternoon (2/5/23), we rode over Daisy Pass in hopes of seeing the recent skier triggered slide on Fisher Mountain, but it had started snowing and visibility was too limited to see the crown or get to the slide. We rode around the back of Fisher to Lulu Pass and then up to the south shoulder of Scotch Bonnet to dig a pit. There was an old, large pile of debris at the bottom of one of the Rasta Chutes that I assume slid last weekend.

We dug a pit at 9,600' on a southwest facing slope. HS was 160cm. Below last weekend's snow (1 foot/30cm deep) was a 10 cm thick layer of soft facets (F+ hardness). We had an ECTN 21 and ECTP 21 on this layer. The recent skier triggered avalanche on Fisher probably broke on this layer, on a more wind-loaded slope. This layer will be a problem for a while, especially as it gets loaded by more new and wind-drifted snow.

Wind was moderate out of the southwest-west, and at 4pm there was 3" of low-density new snow.

ECTPX in two pits at the top of Texas Meadows. No active wind loading. 

We observed some crowns from recent slides just south of the Flanders Peak east glade while touring up Flanders today. The snow was wind affected and slabby especially towards the ridges. No other signs of instability observed. We opted to stay in the trees and minimize exposure on the ski descent.

Heading up the Genesis gully towards Zack Attack on 2/5, we turned around after finding multiple very reactive slabs. The first slab broke very easily, ~4 hits from the wrist, and had a very clean shear ~4in deep. The second slab was more difficult to trigger and did not have a clean shear, but was maybe ~1.5-2ft deep.