Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Your primary avalanche concern today is wind drifted snow that exists near treeline and above on slopes that face NW-N-NE-E-SE. Old hard slabs from strong Southerly winds earlier in the week still remain in alpine terrain. Older, hard wind slabs can be very stubborn. and may not release until you get well out on them. Hard drifts often produce hollow drum-like sounds when you walk on them.
In addition to these lingering hard slabs, fresh slabs formed on Wednesday during the recent storm. Freshly formed wind slabs can be quite sensitive and are more easily triggered. You can recognize them by their smooth, round appearance. Drifted snow is stiffer and more compact than non drifted snow. You will often see clues like cracking in the snow surface when you step onto a recent wind drift.
Large cornices above North facing terrain. These are obvious clues that this slope has seen significant wind loading.