Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
You’ll find recently formed slabs of wind drifted snow in the eastern ravines up to a foot thick. These slabs remain somewhat soft and potentially reactive to a human trigger. The potential exists for larger, thicker slabs tucked here and there on the west side of the range, and in the north including King’s Ravine due to recent higher snowfall totals.
These wind slabs are best described as islands of snow on an icy frozen snow surface, not a complete covering of snow everywhere. In many locations the new snow is very thin or non-existent. What remains is the older refrozen bed surface responsible for multiple skier sliding falls over the last two days with serious injuries as the result. (See Discussion Below)
This avalanche problem may be an attractive surface to climb and ski but remember the unforgiving surface just beneath this new snow. If the lighting is good, the snow surfaces can be easy to identify: new snow will be white, clean while the icy refrozen old surface will be slightly grey color and reflective at obtuse angles to the sun.