The snotel data for Mores Creek summit suggest that the average SWE and precipitation might be reached during the next 24-48 hours as a storm arrives during the night. Although the ski lines above the 7,000 feet are fine, the ski out can made more fun (read less BRUSHY!) if average snow depth is finally reached. Last time, as I was coming out of Freeman, a snow bridge collapsed under me. I do not know what was funnier; the visual of last third of my ski/skins encrusted in ice and snow or my "cat like" skin-up from the creek banks! More snow will make the snow bridges above Mores Creek more reliable.
I decided to tour Winter Corner since I was limited in time. But I also wanted to get snow pit data from a NNW exposure at 7,000 feet. Below a picture from the top of Winter Corner looking to the north. This ski line drops 1,000 feet, where the top is an open slope and the lower half wide spaced old growth forest.
This snow pit is almost identical to the snow pit data shared in this blog for Freeman peak last December 28th. The new 20 cm of snow was today's trail breaking and riding surface. Both snow pits were to the ground, thus the snow depth went from 1.2 to 1.4 meters.
Two compression tests failed failed today (CTM11-Q2, CTM12-Q2) at the basal facet layer 10 cm above the ground. Extended Column Tests (ECT) for fracture propagation did not failed, most likely due to the weak layer exceeding the 1 meter depth. I did not conducted the Propagation Saw Test (PST) for fracture propagation, but based on the PST performed at Freeman Peak few days ago, I expected same results - a very energetic fracture propagation. Below a picture of the second column about to be tested.
During the two CT tests the full columns were displaced approximately 3-4 cm. See the picture below for the displaced column. The tests were conducted on a 28 degrees slope. It is possible that a similar test on a steeper slope would have fully displaced the column, deserving a Q1 rating. However I rated the energy (quality of shear) as Q2.
Another compression test was conducted but with a column isolated only to a meter in depth. The result was CTH24-Q3 on a storm interface at 90 cm formed during the December 26th storm.
The pause in storms have allowed the snowpack to adjust to the sudden snow loading and warm temperatures have allowed for the the sintering of the snowpack. It is reasonable to expect that it will be more difficult to trigger the weak facet layer buried at 1.3 meters considering its depth, and the bridging effect of the denser snow above. Not many places in Mores Creek are steep enough and at the same time lack the ground cover to be able to trigger deep slab avalanches, but be very picky. I suggest a HIGH dosis of prudence and caution as it is NOW easier travel farther. I expect some of the mini-cirques at the 8,000 feet elevation to be spooky - to say the least.
I will be looking forward to see many of you next year.
Happy NEW year! And may the new year bring many face shots days, and many years of good health to all of you.