|My new POW tool!|
The Snotel at Mores Creek Summit reported a whopping 75 inches, an increase in excess of 48 inches (4 feet!). It was no surprise that some pull-outs were not plowed (such as Winter's Corner), and that the parking area at the Summit was limited in parking space. With very few options available I decided to make few laps at Freeman. There was another party at Freeman that selected to put an uphill trail on the main ridge. I still was not sure there was not going to be combat with the brush approaching from the ridge, and opted to built a second uphill track close to a run some call "Elevator" (ski line dropping to the switchback). As expected, trail breaking required more work due to the unconsolidated nature of the new snow.
No whumpfing, cracking, or other sign of instability were present during the climb and approach via a NE subtle ridge to the 7000 feet level. During the drive, and ski touring, crown fractures were visible at SW, W, NE, NW, and N aspects. The fractures appeared to be 25-30 cm deep that ran during the storm cycle only at very steep 37-39 degrees slopes between 6000-7000 feet. Terrain above 7000 was obscured and/or not visible. NO avalanches were observed that might have run on the old snow interface.
|Some brush still poking out even with 4 feet of new snow!|
|Mores Creek Summit Winterland|
I was very fortunate that the camera worked early in the day, and allow me to record the PST (Propagation Saw Test) and Ct (Compression Test). After finishing the the snowpit, my Nikon point & shoot refused to work - it reported a "lens error". Too bad, since it did not allow me to document the several areas with crown fractures.
Below a video for the PST test in a 26 degree slope with East aspect. As you will notice in the video, I was surprised by the propagation at the interface between the New snow and old facet layer (~65 cm from the ground) after just sliding the saw )blunt side) less that 5 cm. The slab experienced a sudden collapse after the propagation, suggesting a Q1 score.
The next video is for the compression column test. A previous test, not recorded resulted in a CTVQ1, or column failure during isolation. On this video, a second column was isolated and failed after just placing the shovel blade in top of the column, perhaps between a CTV and CT1Q1.
This was a surprise to me, to find the deeply buried facet layer so sensitive at relatively low elevation (6800 feet) and after being buried so deeply (1.3 meters) by a slab.
|Snowpit: New snow from 65 to 195 cm|
Between 65 and 155 cm the snow was 4 finger hard, and fist hard from 155 to the surface at 195 cm. A very thin and delicate rain crust was present 20 cm below the snow surface.
The weak layer - a fist hard 2 cm layer of large facets - was found above the pencil hard ground to 63 cm old snow layer.
The snow pit work did not detected any remarkable or reactive layer in the new snow (top 1.3 meter). While skiing down in terrain 30-32 degrees, no new snow surface instabilities were detected, and ski cutting in wind loaded and steep roll-overs did not produce results.
Considering that evidence of "deep" instability was found:
- high probability for trigger likelihood (Easy CT scores)
- high probability for fracture propagation (PST 5/100 End)
- high likelihood of slip after fracture nucleation and propagation at a depth of 1.3 meter (Q1 Scores)
Last weekend a second Avalanche L1 course was completed by Pedro and I. We had a good time at Freeman on Saturday, and a fabulous day at Banner Summit on Sunday.
|Students at Freeman (Top) and Avi Instructors demonstrating companion rescue.|
|Carl 3X - enjoying the turns last Sunday!|
|Carl and Judy gathering data.|
|Pedro with a couple of students at Banner Summit|
I would like to take a few lines to congratulate the students that completed the AVI L1 course last MLK weekend. And knowing that they enjoy this blog, I will include few pictures below for their enjoyment. Thanks Judy for the PICS!