This was our first trip into this area this year. I observed evidence of widespread avalanche activity that likely occurred during the 12/1 avalanche cycle, as well as a few large avalanches that likely occurred 12/4 or 12/5 with additional snow and wind. A very weak snowpack exists in this area, similar to what has been observed across our forecast area.
Clear skies and moderate westerly winds in the White Clouds today, moving small amounts of snow around. Clouds were building in from the south and west throughout the day, limiting solar radiation in the Sawtooths/W Smokys/Banner areas and the Boulders later in the day.
# | Date | Location | Size | Type | Bed Sfc | Depth | Trigger | Photos | Details |
---|---|---|---|---|---|---|---|---|---|
1 |
Dec 5, 2022 (+/- 3 days) |
Fourth of July W 9800ft |
D2.5 | HS-Hard Slab | N-Natural | Report | |||
1 |
Dec 5, 2022 (+/- 3 days) |
Champion Basin NW 9700ft |
D2.5 | HS-Hard Slab | 4ft | N-Natural | Report | ||
3 |
Dec 1, 2022 (+/- 1 day) |
Fourth of July NE 9500ft |
D2 | SS-Soft Slab | N-Natural | Report | |||
1 |
Dec 1, 2022 (+/- 1 day) |
Fourth of July NE 9400ft |
D2 | SS-Soft Slab | N-Natural | Report | |||
2 |
Dec 1, 2022 (+/- 1 day) |
Fourth of July NE 9400ft |
D2 | N-Natural | Report | ||||
25 |
Dec 1, 2022 (+/- 1 day) |
Fourth of July NE 8000ft |
D1.5 | N-Natural | Report |
HS=45-55cm along valley floor at mouth of drainage, increasing to 80-90cm as you get further back in the drainage and climb in elevation. 11/27 weak layer is down 45-50cm here, similar to what has been observed in Galena Summit area. However, the slab here is denser, with a 10cm interval of 1F in the middle. This was enough to easily keep me above it when trail-breaking on skis. On the sled I was floating above it unless I hit the throttle or dug a ski in for a turn. The ability of the slab to keep me above the weak layer made collapsing less common than I've seen in other places recently (the day before in E Fork, and the day before that on Titus), but I still triggered some long traveling collapses and felt that the potential for remotely triggering slides was easily on the table and traveled accordingly. I experienced collapsing and associated cracking in many areas I traveled through, but it was not continuous throughout my tour. In places, slopes did not collapse until my second pass as I returned on the skin track. As I motored in on the sled I could see collapses propagating across meadows and shaking snow off trees.
I found a good bit of SH at the 11/27 interface, but the main problem seemed to be the very weak (F-) facets underneath. The weakest portion of this snow was 5cm thick, but it looked fairly ugly below that as well. I also found remnant snow from October storms (this is our 11/1 interface). This snow had fully made the transition to DH, with large cupped and striated crystals. This snow is very weak, but there isn't an obvious interface between this snow and the weak snow above, its just all weak and ugly. At the ground (as observed in other locations that 11/1 exists), there is 3-5cm icy cap on the ground. This was ever so slightly moist where I dug at 8,200' on a N aspect. This pit returned ECTPV and ECTP5, and CPST 12 and 14/100 both to END. All tests failed on 11/27, down 45-50cm.
Problem | Location | Distribution | Sensitivity | Size | Comments |
---|---|---|---|---|---|
Persistent Slab |
|
Weak Layer(s):
Nov 27, 2022 (FC)
Comments: Rose shaded based on where this weak layer exists. I expect it is at its worst on NW-N-NE-E but I have no interest in gambling with it on the other half of the compass either. Tough call on sensitivity, but based on time since loading and long-traveling collapses I'd put it somewhere between stubborn and reactive. |
"Simple" wind slabs likely exist as a separate problem, but I did not encounter them anywhere that 11/27 didn't exist.