Still there. The October basal facets, while dry, have a tendency to stick together well when squeezed and they don't come pouring out of the pit wall. They are 1.5mm in size and 4F in hardness. Test results in the forested mid-elevation terrain visited did not produce consistent sudden fractures nor did they show a propensity to propagate in our large column tests. Evidence from previous days explosives testing in high elevation Northerly facing terrain also did not yield any avalanches. This somewhat surprising, but not out of the ordinary with a persistent weak layer such as this. As one colleague pointed out, it may take another significant widespread loading event such as a 2-3" H2O storm to really test this layer across the range. In the core of the Cottonwoods and upper most AF canyon where the snowpack is deeper, we may be turning the corner towards increasing strength and improved stability, but the periphery is still suspect. Unsupported slopes and terrain features with underlying rocky convexities also have a high index of suspicion.

Noted winds at the highest ridge line (Timp, Silver Creek, Hidden Peak) were enough to transport snow. The variety of wind directions over the last 24 hours from N to S lead us to be considerate of the upper elevation starting zones and to be aware of the effects of terrain influence on loading patterns.