Thus, we promptly parked at the Bull Trout pull out, exchanged topo maps to the right one - Copper Mountain topo map. We were thrilled to be in the tails of Chris Johnson and his faithful companion, Andrea. No breaking trail for me in the morning!
|Bull Trout Pull-Out, Steven getting ready
|Bull Trout Point in the background
The coverage above 7500 feet is pretty adequate at all aspects, but some care is required to avoid buried obstacles. At all aspects, the coverage below 7500 feet is about 20-30 cms, and my party as well as other reported contact with stumps and rocks.
Temps close to zero degrees Celsius yesterday afternoon below 7500 feet of elevation greatly helped in settling the recent snow, and this process should continue early this week. The snowpack settlement at lower elevations will provide for an adequate base layer for the next precipitation event forecasted later this week.
Temps at the 8000 feet stayed cool all day - right in the minus 4 degrees Celsius, and a light breeze from the NW. The top 20 cms of new light density snow remained fluffy all day long.
|Andrea good looking skiing
The snowpack at 8400 feet in a SW (260 degrees) is summarized next:
Notice the increase in hardness as depth progressed from 20 to 40 cm. The old snow layer at 40 cm produced moderate scores for trigger and slip (CTMQ2) and no propagation potential. During one of the multiple compression tests, one failure occurred at the 60 cm depth, with a "sudden collapse", but it should be noted that the sliding plane was very poor, thus I regarded the fracture plane quality as a Q3.
This might sound like indoctrination, but it is important for BC skiers to recognize structural weaknesses in the snowpack. I am sorry to bore most readers, but for the benefit of some I will highlight the FOUR lemons that can be identified in the above snowpit profile:
- L1: Weak Layer (WL) < 1.0 meter in depth
- L2: WL < 10 cm in thickness
- L3: Slab is present above WL
- L4: WL = Persistent Grain Type (PGT) = Facets
Some avalanche professionals track the hardness of the sliding plane as a "six" lemon, or snowpack structural weakness. It is worth highlighting that for the weak layer at the 50-60 cm depth, there was not a well defined sliding plane due to facet decomposition of the crust layer at the 60-70 cm depth.
In summary, with the combined results at 40 and 60 cm depths, we assumed moderate likelihoods for avalanche trigger, and slab slip if an avalanche was triggered. Considering the previous moderate likelihoods as well as the structural weaknesses of the snowpack (Four lemons) at the 60 cm depth along with its spatial variability, we only skied slope with angles below 34 degrees.
No other evidence of instability was observed through-out the day; no cracks, local collapse, whumpfing, nor during testing of steep and small slopes (non-reactive).