22-23

Obs 12/17: "Saturday afternoon on the way back into town snow was moving in the Spanish peaks. Nice light" 

From obs: 12/16: "I thought this would be interesting to share but while driving around Gallatin gateway today I noticed multiple small wind pockets that released in steep draws in the gateway foothills area." Photo: M. Gaffney

Pit was dug at 8,170'

White Elephant drainage above White Elephant snotel @ 8,170'.

We rode in and toured up the Throne. We dug a pit low, on a northeast aspect at 7,850' and the snow depth was 63cm (2 feet). We had an ECTP27 break on 2-4mm facets at the bottom of the snowpack.

We dug a second pit on the north-norheast facing slope above The Throne at 8,400'. Snow depth here was 95cm (3 feet). We found similar 2-4mm facets making up the bottom 45cm of the snowpack, but we had ECTX 3 times. We were surprised it didn't break or propagate. Despite these test scores, we figured recent snow, wind and a large skier triggered avalanche yesterday were signs to avoid steep slopes, especially if they are wind-loaded.

The sugary, weak facets we found may not yet be showing signs of widespread instability, but combined with more new or wind-drifted snow they could create larger avalanches.

Went into Beehive basin today with a group of people. We dug a pit on a south west aspect just above Beehive meadows at 8384ft to see what was going on in the snow. We got an ECTX for our results.

My partners and I began a tour today at Hyalite Reservoir with a plan to ski the E and N faces of Mount Blackmore, but with the mindset of keeping expectations low and moving slowly giving time for observations and discussion. 

On our way in, just off the trail in an opening in the forest at 8600' on a NW aspect with an incline of 29 deg we chose to dig a test pit mostly to see if a faceted weak layer might be present on the shady aspects we were planning to ski. The pit showed a fully right side up snowpack with the snow progressively going from F hardness new snow to 1F snow towards the ground and a depth of 110cm. The snow was not wind loaded on the surface at our pit location and our ECT yielded an ECTX and no obvious signs of instability. As we climbed towards Blackmore and subsequently ascended the NE ridge, there were occasional gusts on the ridge that were actively blowing snow. The ascent towards the Blackmore summit only presented small shooting cracks and considerable cohesiveness in the surface snow in an isolated pocket towards the summit. 

We opted to ski both the E and N faces and did not notice any instabilities while skiing the lines themselves.

Skied Mt Blackmore today. Dug a pit at 9550ft on a SE facing, 23deg, slope adjacent to the standard east ridge up-track. HS150cm. No wind effect on the surface. 

Had a CTE and CTM on density changes in the top 40cm, ECTN on the same layers.

Pulling the CT block into the pit, the bottom 100 cm was very well bonded and pulled up dirt from the ground with it.

Skied numerous laps, and did not observe any signs of instability. The skiing was excellent.

Went on a tour today with a buddy and traveled through twin falls basin as well as the maid. We skied a NW slope off of Palace Butte and found touchy conditions below the ridge line, but great skiing in the trees. We also skied the bowl of Arden peak. We observed numerous recent wind slabs that released naturally in the past 24 hours on NE and E aspects with some crowns starting to get covered up throughout the day. Judging from afar, I would estimate these crowns to be 6 inches to 1.5 feet deep.