Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
In near and above treeline areas, dense wind slabs have formed during yesterday’s storm cycle. These wind slabs still exist in wind exposed open areas, near ridges, and in gully features. While these wind slabs are showing signs of gaining strength, they still may be reactive today in some areas. Large cornices have built out along ridgelines and could remain fragile.
Look for cornices above slopes, wind pillows, and any cracking or signs of wind slab formation when moving into near and above treeline areas. Move carefully around these areas of concern. Better snow quality will exist in more wind protected terrain away from the denser wind textured snow.
(2/15/2024)
Natural cornice collapse and wind slab avalanche near Frog Lake Cliffs, Donner Summit area.