Old drifts of wind blown snow remain a concern for today. The most likely place to trigger an old lingering wind slab will be on steep, upper elevation, north through easterly facing terrain. Wind drifted snow can be highly variable, and it's typically found on leeward slopes, in gullies, open bowls, and on mid slope breaks-overs. As always, be on the look out and avoid pillowy, rounded, hollow sounding snow. These old drifts of snow are becoming more and more stable as time goes on. Many riders tested the steepest lines and couloirs throughout the Wasatch yesterday with no problems.

New drifts of wind blown snow: The northerly wind could drift the newly fallen snow onto lee aspects creating shallow and sensitive soft slabs in the wind effected terrain. Slope cuts and terrain management skills should be enough to reduce the risk of being caught in one of these smaller slides.

Our buried weak layers are becoming a thing of the past as the snowpack in the central Wasatch continues to grow. However, we can't forget Saturday's human triggered slide that failed on faceted snow. This was probably an outlier but, it's a good example of the type of terrain where it's still possible to trigger a slide that breaks into deeper weak layers. It's likely it will take a large trigger to awaken this dragon such as a cornice drop or a wind slab that steps down deeper in the snowpack. There continues to be an isolated chance that you could trigger a deeper slab avalanche. The most likely spot would be a steep, shallow, rocky slope, that faces north through east above about 9,000' in elevation.

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CORNICES ARE ENORMOUS. Most of these are too large to intentionally drop onto a slope below. They will break back farther than you think, well back from the apex of the ridgeline. Exercise great caution along and underneath the heavily corniced ridgelines.