Avalanches:
Weather: Obscured and overcast sky. Snowfall rates were mostly in the S-1 to S1 range, but rates picked up for an hour here and there to around S2. Calm winds with no new drifting snow observed.
Snowpack: In general, the Thanksgiving Storm and following large storm around 11/26 were creating a nice looking homogeneous snowpack. Any layers of concern or potential layers of concern were near the ground, having formed during the shallow or non-existent snowpack before Thanksgiving. No obvious signs to instability while traveling through east to south to southwest facing slopes. Ski Pen around 25cm.

Dipped into the top of one north facing slope at 11,200ft. Nothing new, HS 130, progressively harder snowpack with depth (F to 4F+) over about 18cm of dry, large facets. The ground cover at the base of the snow pit wasn’t perfectly planner and had some variation in depth due to rock outcrops. Though thats probably representative of the ground cover across the terrain. ECTP 22 SC, ECTN.

East facing 34 degree slope at 11,200ft. HS 140. Same structure as above with the basal facet layer at about 10cm thick, 4F- hard, and both smaller and moist then on the north facing observation.

Avalanches: no avalanches or signs of instability observed except for very minor new snow sloughing in extreme terrain.
Weather: Orographic snow all day, heavy at times. 10-20cm new snow. very light northwids at ridgetop, otherwise calm winds
Snowpack: Very impressive, generally good structured snowpack on all aspects but northerly. Many pits on NE, N, NW, E, and S facing slopes ATL. Generally 120-160cm snowpack with fist to 1 finger hardness snow descending until last 10cm near ground on northerly slopes. Last 10cm consisted of 3mm striated depth hoar. Specifically looked and stomped on steep, northerly terrain with no signs of instability, and good structured snowpack. One profile dug on S-facing slope at 11,500ft, had one mid-pack concerning crust, almost a greenhouse crust, with some very small associated facets.

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Avalanches: See photo. Two small, D1 to D1.5 slides on E face of Mineral Point. One crown visible.
Weather:
Snowpack:

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Avalanches: None seen
Weather: low 20’s, light snow off and on, slight breeze out of southwest, zero snow transport
Snowpack: 2-3 feet deep, ski pen 12 inches, boot pen to the knees. Collapsing at the top of steep roll overs (35-40 degrees), big enough to shake snow off trees, large cracks but nothing moved. Collapsing in flats as well

Avalanches: Investigated 2 crowns of recent remotely triggered avalanches. See photos. Extended column tests produced hard to additional loading propagating results on 1mm facets near the ground, with spotty crust distribution above the weak layers.  Slabs ranged from 40 cm to 100 cm 4F to P hardness, depending on wind effect.
Weather: Overcast skies. Light SE winds. Light snowfall.
Snowpack: Snow depths increased from 25-30 cm below treeline, up to 130 cm in the heaviest wind drifted features above treeline. Near and below treeline, the snow was generally too incohesive and shallow for avalanche concerns; the potential exception would be heavily windloaded features. The base of the snowpack is comprised of 1mm facets, and there was some very small and localized collapsing on this layer near treeline. Above treeline, this same basal weak layer exists, with more of a cohesive slab above, ranging from ~40 cm to ~100 cm

Avalanches: Saw a few old, blown-in crowns out in the distance of Baxter Basin and the north face of Cascade.
Weather: Day started relatively warm (10-15f) and continued to warm as the day went on. Partly cloudy skies began to creep in before the noon hour and by 1-2 skies became more overcast. Wind picked up a little bit in the afternoon but snow transport was very minimal. Definitely had a few instances of getting ‘greenhoused’, and saw some roller balls. Otherwise, sun’s impact on snow was limited.
Snowpack: Snowpack seems to be settling well. Ski pen is around 15-20 cm. Pack grew from 60-70 cm on E and NE slopes towards the valley floor to around 110-120 cm getting closer to treeline. Mostly right-side up, with a small crust-facet combo found in the basement of our NE facing pit at around 11,200 feet. CT21 and CT24, both Q1 shears at around 75 cm from the bottom. Weak layer was hard to identify from the pit wall, I imagine it was either a small layer of near-surface facets or surface hoar; did not notice much of a density change at the weak layer. Otherwise, no signs of instability noted.

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