Despite weak snowpack structure no avalanches nor collapsing/cracking were observed due to low snow volume. I anticipate that a significant winter storm would lead to avalanches and cracking and collapsing on this weak snowpack. The primary hazard continues to be shallowly buried obstacles.
The new snow varied greatly with elevation; about 1 inch was found at 11,100 feet and about 4 inches at 11,800 feet. The snow was dense and contained some rimed particles. Santa Fe SNOTEL showed 4 inches of new snow and about 0.7"of water! Ridgetop winds were moderate from the W-NW. Winds were calm below ridgetop. Minimal snow transport was observed.
Despite traveling on a poor snowpack structure I did not experience collapsing, cracking, nor signs of avalanches. I attribute this to a lack of a slab. In isolated and extreme terrain features one may be able to find a slab over this weak snowpack.
The highly variable shallow snowpack was generally 10 inches deep but ranged from 1-18 inches. The snowpack was made of depth hoar, a melt freeze crust from the December warmth, near surface facets, and about 1-4 inches of new snow. Ski penetration was 2-6 inches. Boot Penetration was full depth.
Persistent weak layer exists, but slab is hard to find. Persistent Slab may exist in extreme and isolated terrain features. No other avalanche problems observed.
I avoided avalanche terrain and targeted shaded slopes that held early season snow to allow for ski travel. I stayed on low angle slopes to avoid higher speed turns in the shallow snow. I had good skiing on low angle slopes, 10-20 degrees, that contained a base of hardened early season.
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